gc: A Pathfinder

This is a computer-generated pathfinder created against the Distant Reader study called gc.

Each Distant Reader study carrel is composed of many individual items. Each item is bibliographically described with author, title, date, summary, and keyword values. Below is a list of the items' most signficant keywords as well as lists of the items themselves. Purpusing the content of this pathfinder provides the student, researcher, or scholar with one way to get their heads around the scope of the carrel. The keywords include:

Area; Deposits; Zagreb; Samples; Basin; Rocks; Water; Carbonate; Data; Species; Formation; Sediments; Croatia; Section; Zone; Geol; Croatica; Miocene; Cretaceous; Middle; Sample; Facies; Values; Adriatic; Karst; Ore; Groundwater; Mineral; Soil; Analysis; Triassic; Type; Croatian; Jurassic; Oil; Geologia; Model; Limestone; Beds; Quartz; Level; Permian; System; Reservoir; Pleistocene; Dinarides; Composition; Specimens; Cave; Sand; Calcite; Algae; Herak; Gas; Barite; Exploration; Region; Sava; Time; Fraction; Branches; Slovenia; Column; Kochansky; Sections; Tion; Stress; Pamić; Structure; Ihe; Lika; Crystals; Evaporite; Speleothems; Specimen; Prof; Sam; Paper; Leaf; Cleal; Management; Edi; Needs

Depending on how this pathfinder was created, many of the bibliographic sections will include elaborations on the meaning(s) of the given keywords. These elaborations were generated by feeding the items' summaries to a large langauge model and asking the model to address the question, "What is X?", where "X" is the keyword. The result will be a few sentences of elaboration. Be forewarned. The elaborations are often plausible, but they should not be take as truth. Instead, they should be taken as points for consideration.

• Assessment of the Geotouristic Values of Devil's Town, Serbia by Vukoičić, Danijela; Srećković-Batoćanin, Danica; Valjarević, Aleksandar; Ristić, Dušan; Nikolić, Milena; Valjarević, Dragana (2021) - Additional natural values Number of additional natural values in the radius of 5 km (geosites also included) 15. Nevertheless, the Stob pyramids occupy a higher position in the matrix due to higher additional values. Keywords: area; assessment; devil; doi; et al; gam; geoheritage; geosite; geotourism; gs2; gs4; hose; level; melnik; number; protection; pyramids; sand; serbia; stob; tomić; town; values; visitors
• Linear features on karst surfaces: an example from Krk Island by Šegina, Ela; Benac, Čedomir; Šušteršič, France; Knez, Martin; Čar, Jože (2021) - Linear features on karst surfaces: an example from Krk Island 147 sists of alluvial sediments on the floor of linear features (Figure 12 A), traces of the erosion as pools, smooth rock sculpturing on the floor of the features and eroded talus breccia (Figure 12 B, C), and the occurrence of alluvial fans at the mouth of linear fea- tures (ŠMUC et al., 2015) Less commonly, a geomorphological investigation has focused on linear features on karst (MILOJEVIĆ, 1955; MON- ROE, 1964; ROGLIĆ, 1964; BROOK & FORD, 1978; DAY, 1983; FAIVRE, 1994; HEVESI, 2001; TÎRLӐ & VIJULIE, 2013; BOČIĆ et al., 2015; HARMAND et al., 2017 etc.). Keywords: area; benac; croatia; doi; et al; features; figure; island; karst; krk; krk island; linear; linear features; runoff; sea; surface
• Natural Resources Self-Sufficiency – How to Balance Groundwater Protection and Mineral Resources Exploitation – Pleterje Case, Slovenia: Legal and Geological Aspects by Pličanič, Senko; Pogačnik, Željko; Koren, Eva; Vižintin, Goran (2021) - Fisica de la Tiera, N°7, 53–86 DUBIŃSKI, J. (2013): Sustainable development of mining mineral resources.– Journal of Sustainable Mining, Vol. 12, No. 1, 1–6. INTRODUCTION Slovenia features multiple alluvial plains that are naturally con­ ducive to the exploitation of mineral resources: two are located in north eastern Slovenia, specifically the Mura and Prekmurska Plains (Mursko polje and Prekmursko polje); next there is the Drava and Ptuj Plain (Dravsko polje and Ptujsko polje) and finally the Krško and Brežice Plain (Krško polje and Brežiško polje) in eastern Slovenia. Keywords: act; area; article; case; constitution; decree; drava; exploitation; figure; government; groundwater; limitations; mineral resources; mining; mining right; model; plain; property; protection; ptuj; right; slovenia
• Paleoecological and sedimentological characterisation of Middle Miocene sediments from the Hrvatska Kostajnica area (Croatia) by Grizelj, Anita; Milošević, Monika; Bakrač, Koraljka; Galović, Ines; Kurečić, Tomislav; Hajek-Tadesse, Valentina; Avanić, Radovan; Miknić, Mirjana; Horvat, Marija; Čaić Janković, Ana; Matošević, Mario (2020) - Arg 18 18 16 13 CLAY 34 36 40 60 31 35 <63 µm Qtz XX XX XX X XX XX CLAY XXX XXX XXX XXX XXX XXX Cli/Hul + X X X X Pl X X X X + X Py X <2 µm Sme/I-S XX XX XX XX XX XX Ill/Ms XX XX XX XX XX XX Vrm + + Kln X X X X X X Chl + + + Qtz + + + + + G eo lo gi a C ro at ic a Geologia Croatica 73/3158 covite are well represented in all samples, while kaolinite is pre- sent in all samples in a lesser quantity (Tab. 1 and Fig. 4). In contrast, the Badenian/Sarmatian boundary is discon- tinuous in many cases within Central Paratethys (VRSALJKO et al., 2006; MANDIC et al., 2019b; MANDIC et al., 2019c). Keywords: area; badenian; basin; bolivina; column; croatia; d'orbigny; doi; environment; et al; fig; foraminifera; geol; hrvatska; kos; kostajnica; late; marine; marls; middle; miocene; paratethys; pavelić; rocks; samples; sarmatian; sediments; species; x x
• Spatial distribution and geometric characteristics of landslides with special reference to geological units in the area of Slavonski Brod, Croatia by Bostjančić, Iris; Avanić, Radovan; Frangen, Tihomir; Pavić, Mirja (2022) - The landslide index, expressed in percentages, is cal- culated as a ratio between landslide area in a given GU and the area of that unit. The distribution of landslide area is presented in more detail via the frequency den- sity and a cumulative number of landslides (Fig. 5). Keywords: area; characteristics; classes; density; distribution; doi; et al; gu4; gu5; landslide; landslide area; landslide density; relief; slope; study; study area; units
• Mineral assemblage and provenance of the Pliocene Viviparus beds from the Area of Vukomeričke Gorice (Central Croatia) by Kurečić, Tomislav; Kovačić, Marijan; Grizelj, Anita (2021) - This period is also characterized by strong volcanic activity (MANDIC et al., 2012; PAVELIĆ & KOVAČIĆ, 2018; BRLEK et al., 2020; MARKOVIĆ et al., 2021). Today it is known as Lake Slavonia (HARZHAUSER & MANDIĆ, 2008; MANDIC et al., 2015; NEUBAUER et al., 2015). Keywords: area; basin; beds; chemical; composition; croatia; detritus; doi; et al; fig; geol; gorice; kovačić; mineral; miocene; pannonian; pliocene; provenance; quartz; rocks; samples; sand; sediments; tab; viviparus; vukomeričke; zagreb
• The preliminary inventory of coseismic ground failures related to December 2020 – January 2021 Petrinja earthquake series by Pollak, Davor; Gulam, Vlatko; Novosel, Tomislav; Avanić, Radovan; Tomljenović, Bruno; Hećej, Nina; Terzić, Josip; Stipčević, Josip; Bačić, Mario; Kurečić, Tomislav; Dolić, Mario; Bostjančić, Iris; Wacha, Lara; Kosović, Ivan; Budić, Marko; Vukovski, Matija; Belić, Nikola; Špelić, Marko; Brčić, Vlatko; Barbača, Josip; Kordić, Branko; Palenik, Damir; Filjak, Radovan; Frangen, Tihomir; Pavić, Mirja; Urumović, Kosta; Sečanj, Marin; Matoš, Bojan; Govorčin, Marin; Kovačević, Meho Saša; Librić, Lovorka (2021) - high 41 P-NDTV-13a Sand boil 481504 5032582 HGI 05.01.2021. high 42 PE-NDTV-02 Sand boil 481883 5032780 HGI 05.01.2021. Keywords: 05.01.2021; area; boil; croatian; data; doi; doline; dropout; earthquake; et al; failures; figure; geological; ground; hgi; hgi 05.01.2021; liquefaction; map; medium; petrinja; road; rupture; sand; sand boil; sediments; slide; soil; subsidence; zagreb
• Quantity status of groundwater in alluvial aquifers in northern Croatia by Brkić, Željka; Larva, Ozren; Urumović, Kosta (2010) - Keywords: monitoring, groundwater level trend, stages of the Drava and Sava rivers, precipitation The quantitative status of groundwater in alluvial aquifers in norther Croatia � Željka Brkić, Ozren Larva and Kosta Urumović Department of Hydrogeology and Engineering Geology, Croatian Geological Survey, Sachsova 2, Zagreb, Croatia; (zeljka.brkic@hgi-cgs.hr) doi: 104154/gc.2010.23 Geologia Croatica 63/3 283–298 27 Figs. All water gauging stations downstream of the hydro- power plants and accumulation lakes show a trend of lower- ing of Drava water levels. Keywords: aquifer; area; croatia; drava; drava river; fig; groundwater levels; ned; period; piezometers; precipitation; quantities; river; sava; trend; zagreb
• Middle Aptian Orbitolinid limestones in Belgrade (Serbia): microfacies and depositional environment by Đorđević, Bojana; Gawlick, Hans-Jürgen ; Djerić, Nevenka; Schlagintweit, Felix ; Radonjić, Miloš (2023) - Biostratigraphy In the Tethyan realm, the Aptian stage is subdivided into three divisions: Bedoulian (early Aptian), Gargasian (middle Aptian) and Clansayesian (late Aptian) (GRADSTEIN et al., 2020). TOLJIĆ et al. (2018) in the latest paper attributed the Para- flysch sequence to be deposited on the outer passive margin of the Moesian plate (Carpatho-Balkanides), and in the oceanic ba- sin between the wider Adria plate to the west (Dinarides) and the Moesian plate (Europe) to the east. Keywords: age; aptian; area; bdz; belgrade; cretaceous; doi; et al; fig; foraminifera; gawlick; jurassic; limestones; microfacies; middle
• A case study in the research polygon in Glina and Dvor municipality, Croatia–landslide susceptibility assessment of geological units by Filipović, Marina; Mišur, Ivan; Gulam, Vlatko; Horvat, Marija (2022) - Landslide areas were derived automatically, whereas length and width ratios were extracted manually in the ArcGIS environment. Landslide areas in square metres are shown with Box and Whisker plots. Keywords: analysis; area; categories; category; croatian; drainage; et al; figure; landslide; landslide susceptibility; lidar; map; mvim; polygon; relief; research; rocks; study; susceptibility; units; values
• Genesis of ferromanganese deposits from the Central Anatolian province, Yozgat-Aşağı Eğerci village, Turkey: Geochemical properties and fluid inclusions by Öksüz, Nursel; Kaya, Sümeyra (2021) - The Co/Ni ratio is commonly used to understand ore formation pro- cesses in manganese deposits (DELIAN, 1994; FERNANDEZ & MORO, 1998). DEL RIO SALAS, R., RUIZ, J., OCHOA-LANDÍN, L., NORIEGA, O., BARRA, F., MEZA-FIGUEROA, D. & PAZ-MORENO, F. (2008): Geology, Geochemistry and Re-Os systematics of manganese deposits from the Santa Rosalía Basin and adjacent areas in Baja California Sur, México.– Keywords: area; deposits; doi; fig; goethite; hydrothermal; inclusions; liquid; manganese; mineralization; ore; samples; study; turkey; type; values; vapor
• A sedimentological description of the Middle Triassic vertebrate-bearing limestone from Velika planina, the Kamnik-Savinja Alps, Slovenia by Gale, Luka; Hitij, Tomaž; Vičič, Blaž; Križnar, Matija; Žalohar, Jure; Celarc, Bogomir; Vrabec, Marko (2022) - A sedimentological description of the Middle Triassic vertebrate-bearing limestone from Velika planina, the Kamnik-Savinja Alps, Slovenia 103 marlstone, mudstone, thin- to medium-thick bedded limestone and dolomite of the middle to upper Anisian (Pelsonian – early Illyrian) Strelovec Formation which is up to 60 m thick (CE- LARC et al., 2013; MIKLAVC et al., 2016; PRIMOŽIČ, 2020). A sedimentological description of the Middle Triassic vertebrate-bearing limestone from Velika planina, the Kamnik-Savinja Alps, Slovenia 105 Figure 5. Keywords: alps; area; doi; dolomite; fig; foraminifers; formation; grainstone; kamnik; limestone; ljubljana; member; microfacies; middle; mudstone; planina; savinja; section; slovenia; triassic; velika; velika planina; wackestone
• Vulnerability of the karst area related to potentially toxic elements by Fajković, Hana; Hasan, Ozren; Miko, Slobodan; Juračić, Mladen; Mesić, Saša; Prohić, Esad (2010) - Keywords: karst, vulnerability map, PI-method, soil, environmental geochemistry, Una River Vulnerability of the karst area related to potentially toxic elements � Hana Fajković1, Ozren Hasan2, Slobodan Miko2, Mladen Juračić1, Saša Mesić2 and Esad Prohić1 1Department of Geology, Faculty of Science, University of Zagreb, Horvatovac 95, 10000 Zagreb, Croatia; (hanaf@geol.pmf.hr) 2Croatian Geological Survey, Sachsova 2, 10000 Zagreb, Croatia; (slobodan.miko@hgi-cgs.hr) doi: 104154/gc.2011.04 Geologia Croatica 64/1 41–48 2 Figs. DISCUSSION AND CONCLUSION Two types of maps, the PI-map (or vulnerability map), and maps of the mobile fraction content of the topsoil cover in relation to the deeper layer, were combined in order to as- sess the potential hazard to groundwater. Keywords: area; elements; karst; loam; map; mobile; n.a; silt; vulnerability
• Preliminary analysis of a LiDAR-based landslide inventory in the area of Samobor, Croatia by Gulam, Vlatko; Bostjančić, Iris; Hećej, Nina; Filipovic, Marina; Filjak, Radovan (2022) - The reason for that could be large landslide polygons delineated within that GU and this assumption is confirmed in Table 1, where the GU Pl,Q is presented as the second one in the rank list of average landslide area for all GUs. Landslide inventory map A total of 874 landslides were outlined within the investigated area. Keywords: analysis; area; croatia; deposits; energy; fig; geological; group; gus; index; inventory; landslide; landslide index; map; relief; scale; study; study area; susceptibility; units
• Use of a LiDAR-derived landslide inventory map in assessing Influencing factors for landslide susceptibility of geological units in the Petrinja area (Croatia) by Frangen, Tihomir; Pavić, Mirja; Gulam, Vlatko; Kurečić, Tomislav (2022) - Landslide index The landslide index is calculated as a ratio between landslide area in a given GU and the area of that GU and is expressed as a in percentage. Frequency density and the cumulative number of landslides considering landslide area. Keywords: area; badenian; data; deposits; doi; fig; gus; inventory; landslide; landslide susceptibility; lidar; map; maps; pliocene; scale; study; study area; susceptibility; unit
• Current utilization and hydrochemical characteristics of geothermal aquifers in the Bjelovar sub-depression by Marković, Tamara; Sladović, Željka; Domitrović, Dragutin; Karlović, Igor; Larva, Ozren (2022) - Increased utilization of thermal aqui- fers has raised awareness of their protection and sustainability, and feasibility studies appeared in the early 19th century in which protection zones and rules on how to behave with thermal waters were defined (BANCALARI, 1868; RAK, 1876; GRUDELJ, 1890; GORJANOVIĆ-KRAMBERGER, 1896). Two differ- ent laws regulate the usage of thermal waters, based on the method of utilization. Keywords: aquifers; area; basin; bjelovar; ciglena; croatian; daruvar; depression; doi; geothermal; pannonian; sediments; spa; thermal; water
• The origin and composition of flysch deposits as an attribute to the excessive erosion of the Slani Potok valley („Salty Creek“), Croatia by Aljinović, Dunja; Jurak, Vladimir; Mileusnić, Marta; Slovenec, Dragutin; Presečki, Filip (2010) - Slani Potok fl ysch is predominantly composed of pelitic intervals, with sub- ordinate sandstones and biocalcirudites. The interrelationship of thenardite and the erosion of fl ysch rocks is two fold: 1) Keywords: area; composition; deposits; et al; fl ysch; potok; sandstones; slani; slani potok; sodium; ysch
• Upper Miocene ostracods from the Krško Basin, SE Slovenia by Marinšek, Miha; Hajek-Tadesse, Valentina; Poljak, Marijan; Kolar-Jurkovšek, Tea; Gale, Luka (2023) - Upper Miocene ostracods from the Krško Basin, SE Slovenia 67 In the comparison, from the literature, we only included Up- per Pannonian ostracod species. Data pre- sented here serve as an important contribution to the understand- ing of the distribution of ostracods in Lake Pannon as the last known scientific paper on Miocene ostracods from Slovenia was published in 1989 (STEVANOVIĆ & ŠKERLJ, 1989). Keywords: area; basin; bizeljsko; central; doi; formation; geološki; krško; miocene; ostracod; pannonian; paratethys; poljak; sample; section; slovenia; sokač; species; view
• Large gravitational collapse structure on a rocky coast (Kvarner, NE Adriatic Sea) by Benac, Čedomir; Dugonjić Jovančević, Sanja; Navratil, Dražen; Tadić, Andrea; Maglić, Lovro (2023) - Rock collapse occurred on an irregular rupture surface consisting of a number of randomly oriented joints, separated by segments of intact rock. The instability studied is a large gravitational collapse structure or rock collapse. Keywords: adriatic; area; benac; coast; collapse; doi; figure; kvarner; level; mass; rock; sea; structure
• Lower Permian Košna conglomerates of the Velebit Mt. (Croatia): modal composition, provenance and depositional environment by Palatinuš, Iva; Gobo, Katarina; Fio Firi, Karmen; Marković, Frane; Sremac, Jasenka (2024) - Lower Permian Košna conglomerates of the Velebit Mt. (Croatia): modal composition, provenance and depositional environment 3 Petrological analyses of conglomerate clasts and matrix were undertaken at the Department of Geology of the Faculty of Sci- ence, University of Zagreb. Lower Permian Košna conglomerates of the Velebit Mt. (Croatia): modal composition, provenance and depositional environment 5 The weathering index diagram (WELTJE, 1994; WELTJE et al., 1998) consists of two areas indicating the origin of the weathered material (metamorphic/sedimentary or plutonic). Keywords: alps; area; clasts; conglomerates; deposits; devidé; doi; environment; et al; fig; kochansky; košna; krainer; limestone; matrix; permian; salopek; southern; sremac; velebit
• Integrated assessment of groundwater quality, agriculture suitability and health risk assessment in the Upper Indus Basin, District Gujranwala, Pakistan by Rehman, Faisal; Razaq, Mishal; Azeem, Tahir; Toqeer, Muhammad; Saeed, Haleema; Siddique, Jamil; Mahwish, Syeda ; Rehman, Faisal; Mustafa, Salman (2025) - The physico-chemical properties of groundwater samples, collected from Gujranwala district are examined through a G eo lo gi a C ro at ic a 132 Geologia Croatica 78/2 statistical summary that represents the concentrations of ions dissolved in groundwater, their comparison with maximum allowed limit proposed by the WHO and other hydrogeological parameters including hardness, pH, turbidity, electrical conductivity (EC), bicarbonates (HCO3 −), chloride (Cl−), carbonates (CO3 2−), sulfate (SO4 2−), magnesium-ion (Mg2+), calcium-ion (Ca2+), potassium-ion (K+), sodium-ion (Na+), nitrate (NO3 −), fluoride (F−), iron (Fe), phosphate (PO4 3−) and arsenic (As). Location map of groundwater samples collected from water schemes in the Gujranwala district. Keywords: area; arsenic; assessment; environmental; et al; groundwater; groundwater quality; groundwater samples; gujranwala; health; pakistan; quality; risk; samples; study
• The role of pollen and NPP research in palaeoenvironmental reconstruction of the Neolithic archaeological site “Gorjani-Topole” (Slavonia region, eastern Croatia) by Hruševar, Dario; Bakrač, Koraljka; Mitić, Božena; Baniček, Ivona ; Šošić Klindžić, Rajna (2024) - The fungus HdV­200, which is common in the sediment formed by the decomposition of helophytes at the bottom of water pools during dry periods (VAN GEEL et al., 1989), further supports the indication that conditions of alternating humidity were pronounced. Moreover, ecological indi­ cator values of particular pollen species highlights temperature changes, hydrological or trophic substrate level in the particular study area and possible human impacts on the environment (COURT-PICON et al., 2006; ANDRIČ, 2007; FEURDEAN et al., 2013; KULKARNI et al., 2016; HRUŠEVAR et al., 2020). Keywords: analysis; area; charcoal; doi; et al; fungal; geel; gorjani; holocene; human; indicators; neolithic; npps; palynology; palynomorphs; particles; pollen; samples; site; spores; suppl; van; vegetation
• Early Jurassic radiolarians from the Weitenau area (Northern Calcareous Alps, Austria) and their implications on palaeogeography by Cifer, Tim; Gawlick, Hans-Jürgen; Krische, Oliver (2025) - Early Jurassic radiolarians from the Weitenau area (Northern Calcareous Alps, Austria) and their implications for palaeogeography (GAWLICK et al., 1999; HILLEBRANDT & KRYSTYN, 2009). Early Jurassic radiolarians from the Weitenau area (Northern Calcareous Alps, Austria) and their implications for palaeogeography marly-siliceous Dürrnberg Formation and to the Toarcian– Aalenian Birkenfeld Formation (GAWLICK et al., 2009; MISSONI & GAWLICK, 2011a, b). Keywords: alps; area; austria; calcareous; carter; et al; formation; gawlick; gawlick et; goričan; haselgebirge; jurassic; missoni; mélange; radiolarian; shelf; w368; whalen
• Hydrochemical characterization of a Dinaric karst catchment in relation to emerging organic contaminants by Selak, Ana; Lukač Reberski, Jasmina; Briški, Maja ; Selak, Lorena (2024) - doi: 10.1016/j. chemer.2011.08.001 MUDARRA, M., ANDREO, B. & BAKER, A. (2011): Characterisation of dissolved organic matter in karst spring waters using intrinsic fluores­ cence: Relationship with infiltration processes.– [Mg2+]/[Ca2+] ratios can be indicative of matrix water or diffuse recharge through the epikarst, whereas lower [Mg2+]/[Ca2+] values observed in spring water are associated with conduit recharge (TORAN & REISCH, 2013). Keywords: aquifer; area; catchment; cetina; cetina river; correlation; data; dinaric; doi; eocs; et al; fig; gizdavac; groundwater; jadro; karst; mean; precipitation; river; samples; springs; values; water; žrnovnica
• Tracing hydrological processes: insights from hydrochemical and isotopic investigations in the northern part of Croatian Dinaric karst by Boljat, Ivana; Terzić, Josip; Duić, Željko; Lukač Reberski, Jasmina; Selak, Ana ; Briški, Maja (2024) - Still, the observed isotope values in Mrežnica spring waters have more negative values than those of the Gojak spring water. The SEC in spring waters ranges between 272 and 506 µS/ cm, with an anomaly noted in December 2019 in the Tounjčica spring, when the SEC measured 659 µS/cm. Keywords: area; catchment; doi; dretulja; et al; gojak; groundwater; isotopic; kapela; karst; mrežnica; precipitation; slunjčica; spring; spring water; tounjčica; values; veliko; vrelo; water; zagorska
• Hydrogeological parameterisation of the Daruvar thermal aquifer: integration of fracture network analysis and well testing by Kosović, Ivan; Matoš, Bojan; Casiraghi, Stefano; Benedetti, Gabriele; Frangen, Tihomir ; Urumović, Kosta; Pavičić, Ivica; Bistacchi, Andrea; Mittempergher, Silvia ; Pola, Marco; Borović, Staša (2024) - In rocks having low primary porosity and permeability, the bulk hydraulic properties are controlled by the network of fractures crosscutting the rock mass (SINGHAL & GUPTA, Hydrogeological parameterisation of the Daruvar thermal aquifer: integration of fracture network analysis and well testing Ivan Kosović1, Bojan Matoš2,*, Stefano Casiraghi3, Gabriele Benedetti3, Tihomir Frangen1, Kosta Urumović1, Ivica Pavičić2, Andrea Bistacchi3, Silvia Mittempergher3, Marco Pola1 and Staša Borović1 1 Croatian Geological Survey, Department of Hydrogeology and Engineering Geology, Sachsova 2, 10000 Zagreb, Croatia 2 University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Department of Geology and Geological Engineering, Pierottijeva 6, 10000 Zagreb, Croatia; (*corresponding author: bojan.matos@rgn.unizg.hr) 3 Università degli Studi di Milano Bicocca, Dipartimento di Scienze dell'Ambiente e della Terra, Piazza della Scienza, 4, 20126 Milan, Italy doi: 10.4154/gc.2024.11 Abstract Highly fractured Mesozoic carbonate rocks are the main reservoir of many geothermal re- sources in northern Croatia, being of environmental, cultural, and economic value for the local and regional communities. Hydrogeological parameterisation of the Daruvar thermal aquifer: integration of fracture network analysis and well testing al., 1998; TARI et al., 1999; CSONTOS & VÖRÖS, 2004; USTASZEWSKI et al., 2010) Keywords: analysis; aperture; aquifer; area; daruvar; data; dfn; dip; discontinuity; doi; et al; fault; field; fig; fracture; hydraulic; hydrogeological; length; model; network; outcrop; pumping; quarry; results; set; system; tab; values
• A conceptual and numerical model of fluid flow and heat transport in the Topusko hydrothermal system by Pavić, Mirja; Pola, Marco; Matoš, Bojan; Mišić, Katarina; Kosović, Ivan; Pavičić, Ivica; Borović, Staša (2024) - The equivalent po- rous medium approach was employed for the hydrogeological and thermal parametrisations of the hydrostratigraphic units (DIERSCH, 2014; ANDERSON et al., 2015). Since it is generally used to simulate the variable outflow in springs (ANDERSON et al., 2015), it was employed in the THS numerical model to reproduce the occurrence of thermal springs in the Topusko area. Keywords: aquifer; area; carbonate; croatian; doi; et al; fault; fig; flow; fluid; geothermal; heat; hydrothermal; model; modelling; numerical; regional; system; tectonic; temperature; ths; topusko; transport; triassic; units; water
• Conflicting tectonic interpretations of the central External Dinarides by Korbar, Tvrtko (2025) - However, BALLING et al. (2023) reinterpreted the Lika fault as a single nappe encompassing the Bruvno dome also from the south, although, even according to the authors, the detachment horizons are different, i.e., the older thrust sheet (northern) was detached at Lower Triassic and was thrust to the south, while the younger thrust sheet (southern) includes also the Palaeozoic strata and was thrust to the north. al. (2020) rather than an older version that had a better fit to the local data (SCHMID et al., 2008). Keywords: area; balling; breccia; central; data; dinarides; et al; fault; fig; geological; korbar; lika; model; tectonic; velebit
• Epikarst of Eastern part of Suva Planina Mt.: a new perspective defining from an integrated survey by Petrović, Branislav; Ignjatović, Snežana; Smiljković, Živojin; Marinović, Veljko; Gajić, Violeta (2025) - Within the framework of land cover (soil) research, parameters of soil samples (S1­S8) were determined in the laboratory: soil moisture, mineral composition, soil organic matter content, as well as the physico­chemical processes that occur within it, influencing the changing properties of surface (ground) waters. Pearson correlation matrix of soil samples analyses. Keywords: area; content; epikarst; fig; layer; limestone; map; mapping; petrović; planina; potential; research; rock; samples; soil; suva; suva planina; water
• Geozonation of the Zagreb city area as an input for seismic risk assessment by Podolszki, Laszlo; Terzić, Josip; Patekar, Matko (2025) - Research area: a Zagreb city area within Croatia; b Zagreb city area topography; c Zagreb city area morphology; d Existing geozonation for Zagreb city area with defined zones (JURAK et al., 2008): I – Medvednica Mt. area, IIa, b, c – slopes of Medvednica Mt. with wider area, and IIIa, b, c – the wider area of the Sava river. Ground types according to Eurocode 8 (A-S2) and ground types in the research area (A-D, ≈ 175 km2, ≈ 1/4 of Zagreb city area) within Zagreb County (HERAK et al., 2013; MIKLIN et al., 2019; PADOVAN et al., 2021) Ground type Description vs,30* NSPT** cu*** Research area (≈ 175 km2) A Rock or other rock-like geological formation, including at most 5 m of weaker material at the surface. Keywords: area; assessment; city area; croatian; data; engineering; et al; ground; map; maps; medvednica; research; risk; scale; sediments; slopes; zagreb; zagreb city; zone
• Historical maps as a tool in the interpretation of urban topsoil geochemistry: A case study from the Roman city of Sisak, Croatia by Pjanić, Ajka; Durn, Goran; Halamić, Josip (2025) - The geochemical maps of the city of Sisak area were generated using descriptive statistics of the concentration of individual elements in the topsoil (ŠORŠA & HALAMIĆ, 2014), as well as using multivariate statistical analyses of the entire set of chemical elements and pH, including factor analysis (ŠORŠA et al., 2017) and discriminant analysis (ŠORŠA et al., 2018a). A geochemical map of the spatial distribution of Au in Sisak topsoil. Keywords: area; city; elements; fig; maps; period; sisak; siscia; study; topsoil; šorša
• Geology and mineralogy of the radioactive Quaternary sediments of the North Fayium depression, Western Desert, Egypt by Raslan, Mohamed Fahmy; Haroun, Yehia Sayed (2010) - raslan&haroun.indd 333 � AB STRA CT Quaternary sediments of the North Fayium depression, are mainly represented by residual soil and calcrete, and have been found to be anomalously radioactive. Trace element analysis in the studied rock types indicates enrichment in Zn, Zr, Y, Sr and V. Keywords: radioactive Quaternary sediments, residual soil, calcrete, zircon, apatite, Western Desert, Egypt Geology and mineralogy of the radioactive Quaternary sediments of the North Fayium depression, Western Desert, Egypt � Mohamed F. Raslan and Yehia S. Haroun Nuclear Materials Authority, P.O. Box 530, EL Maadi, Cairo, Egypt; (ralangains@hotmail.com) doi: 104154/gc.2010.27 Geologia Croatica 63/3 333–343 8 Figs. Keywords: area; calcrete; fayium; haroun; minerals; sediments; shale; soil; study; uranium
• The conceptual hydrogeological model of the Plitvice Lakes by Biondić, Božidar; Biondić, Ranko; Meaški, Hrvoje (2010) - Lake water is generally oversaturated with calcite and dolomite through- out the monitored period. Hydrochemical research has consisted of a total of 3022 measurements of physico-chemical parameters and 7885 analysis of karst spring, river and lake water samples, of which only a small part, in our opinion showing the char- Fi gu re 3: A conceptual model of the genesis of the Plitvice Lakes system. Keywords: area; karst; kozjak; lake kozjak; lakes; lakes system; national; park; plitvice lakes; river; spring; system; water
• Stratigraphy and Palaeobiogeography of Mesozoic Benthic Foraminifera - Part 3 by Velić, Ivo (2008) - Scale bars – 1, 13: 0.5 mm, 2, 6–7, 9: 0.1mm, 3–5, 8, 10–12, 14: 0.2 mm. 89Velić PLATE XIV 90 Geologia Croatica 60/1 PLATE XV 1–5 Mesorbitolina texana (ROEMER), Late Aptian–Early Albian; 1, 3–5: Jajce area, Bosnia and Herzegovina, 2: Ogulin area, Croatia. Scale bars – 1–4: 0.1 mm, 5–10: 0.2 mm. 105Velić PLATE XXII 106 Geologia Croatica 60/1 PLATE XXIII 1–4 Dicyclina schlumbergeri MUNIER-CHALMAS, Santonian–Campanian; 1–2: Jajce area, Bosnia and Herzegovina, 3: Ogulin area, 4: Biokovo Mt., Croatia. Keywords: area; croatia
• Evidence for Badenian local sea level changes in the proximal area of the North Croatian Basin by Bakrač, Koraljka; Hajek-Tadesse, Valentina; Miknić, Mirjana; Grizelj, Anita; Hećimović, Ivan; Kovačić, Marijan (2010) - Miocene sediments are most commonly in tectonic con- tact with Mesozoic carbonates, and less often with Paleogene rocks which constitute a major part of the core of Mt. Samo- borsko gorje (ŠIKIĆ et al., 1979; VRSALJKO et al., 2005). In the Basic Geological map ŠIKIĆ et al., (1979) as sig ned these deposits as did GORJANOVIĆ-KRAM BER GER (1894, 1896), to the “Helvetian” (Ottnangian). Keywords: area; badenian; basin; croatian; facies; fauna; freshwater; marine; middle; miocene; orbigny; ostracod; samples; sea; section; sediments; species; vrhovčak; � �
• New biostratigraphic data from the Early Pleistocene tyrrhenian PALEOCOAST (Western Umbria, Central Italy) by Baldanza, Angela; Bizzarri, Roberto; Hepach, Helmke (2011) - The nannofossil assemblages are attributable to the MNN19c subzone, thus confi rming the presence of Early Pleistocene deposits in the Pod. Palombaro area. Contrary to former palaeogeographic interpretations, the occurrence of Early Pleistocene marine deposits is largely documented in the Orvieto area. Keywords: area; bizzarri; deposits; et al; fig; nannofossil; orvieto; pleistocene; section; umbria
• Hydrogeological Relationships of the Golubinka Karst Spring in Ljubač Bay, Dalmatia, Croatia by Pavičić, Ante; Terzić, Josip; Berović, Nicoletta (2010) - This circumstance is positive from the hydro- geological point of view, because the groundwater flow from the aquifer can suppress the intruding sea water; thus the Golubinka spring water stays fresh until the end of the summer dry periods when the groundwater level in the aquifer drops, together with the discharge, and sea water intrudes. When sea water intrusion becomes excessive at the end of the summer dry periods, pumping has to be stopped. Keywords: analysis; area; catchment; factor; fig; golubinka; groundwater; karst; level; sea; spring; table; water
• The Effect of the Seawater Intrusion on the Robinzon Coastal Spring by Buljan, Renato; Marković, Tamara; Peh, Zoran (2010) - However, data explaining the natural conditions of the Robinzon Spring before the power plant had been built were drawn out from the cadastral sheet of the Duboka Ljuta–Robinzon Spring (PERGER, 19604). Faults with planes dipping R10/74 and R87/82 are dominant in the immediate vicinity of the Robinzon Spring (Fig. 2). Keywords: area; carbonate; depth; fig; flysch; hydrogeological; robinzon; robinzon spring; rocks; seawater; spring; water; zone
• Stratigraphy and Palaeogeography of Miocene Deposits from the Marginal Area of Žumberak Mt. and the Samoborsko Gorje Mts. (Northwestern Croatia) by Vrsaljko, Davor; Pavelić, Davor; Bajraktarević, Zlatan (2010) - Vrsaljko et al..indd Stratigraphy and Palaeogeography of Miocene Deposits from the Marginal Area of Žumberak Mt. and the Samoborsko Gorje Mts. The Plešivica–Sveta Jana area is characterized by a 600 m sequence of Miocene deposits, mainly overlying Trias- sic dolomites, where finely-grained layers of marls and silts prevail. Keywords: age; area; badenian; deposits; figs; gorje; marls; miocene; mts; pannonian; samoborsko; sarmatian; sediments; vrsaljko; žumberak; žumberak mt
• Stratigraphy and Palaeobiogeography of Mesozoic Benthic Foraminifera - Part 1 by Velić, Ivo (2008) - Legend: 1) Pseudocyclammina liassica–Gutnicella cayeuxi interval zone; 2) Gutnicella cayeuxi partial range zone; 3) Timidonella sarda taxon-range zone; �) Timidonella sarda–Pseudodictyopsella jurassica interval zone; �) Pseudodictyopsella jurassica and Marzoella ficcarellii assemblage zone; 6) Pseudodictyopsella jurassica–Par- avalvulina complicata interval zone; 7) Paravalvulina complicata taxon–range zone; 8) Paleopfenderina salernitana taxon-range zone; 8.1) Pseudodictyopsella jurassica and Marzoella ficcarellii assemblage zone Boundaries: stratigraphic ranges of P. jurassica and M. ficcarellii. Keywords: adcp; adriatic; albian; aptian; area; assemblage; assemblage zone; barremian; bathonian; carbonate; cenomanian; conica; cretacea; cretaceous; croatica; cuvillieri; deposits; dinarides; discussion; early; elongata; end; et al; fig; foraminifera; forms; fossils; geol; gušić; index; interval zone; jurassic; jurassic deposits; karst; kurnubia; late; lineage zone; mesozoic; middle; occurrence; orbitopsella; palastiniensis; platform; praecursor; range; range zone; schroeder; sokač; species; stratigraphy; taxa; triassic; velić; vlahović; western; zone; zone boundaries
• Statistical Indicators of Groundwater Geochemical Characteristics in a Quaternary Aquifer from the Mala Mlaka Well Field Catchment Area (Zagreb, Croatia) by Nakić, Zoran; Horvat, Siniša; Bačani, Andrea (2010) - 4. STATISTICAL ANALYSES In the article, time series analysis and multivariate sta- tistical analyses: factor analysis, cluster analysis and multidimensional scaling analysis (MDS ) are used. Factor analysis attempts to simultaneously explain relationships between several variables in order to find more simple relations that ensure an insight into a hid- den data structure (SUK & KANG-KUN, 1999). Keywords: analysis; area; catchment; data; field; fig; groundwater; mala; mlaka; observation; results; wells
• Lower Aptian Rudist Faunas (Bivalvia, Hippuritoidea) from Croatia by Masse, Jean-Pierre; Fenerci-Masse, Mukerrem; Korbar, Tvrtko; Velić, Ivo (2010) - The objective of the present paper is to specify the taxonomic position of Lower Aptian rudists found in the Kanfanar area of Istria, and the Tounj area of central Croatia (Fig. 1). France, 8/5, 715–721. MASSE, J.P. (1992): Les rudistes de l’Aptien inférieur d’italie continentale: aspects systematiques, stratigraphiques et paléobiogeographiques [Lower Aptian rudists of continental Italy: systematic, stratigraphic and palaeo- biogeographic aspects – in French].– Keywords: aptian; area; cretaceous; croatia; et al; faunas; fig; kanfanar; limestones; masse; platform; posterior; rudist; tounj; valve; velić
• Triassic Magmatism in the Area of the Central Dinarides (Bosnia and Herzegovina): Geochemical Resolving of Tectonic Setting by Trubelja, Fabijan; Burgath, Klaus Peter; Marchig, Vesna (2010) - This is not in contradiction with the classification of the other investigated samples as volcanic arc rocks because a wide range of magmatic rocks, from ridge basalts via IAT to calc-alkaline rocks can be associ- ated in zones of former convergent margins, e.g. in Semail, Oman (BEURRIER et al., 1989), Pindos, Greece (BECCALUVA et al., 1979) or Mirdita, Albania (GJATA, 19973; HÖCK et al., 1998). In the Central Dinarides of Bosnia and Herzegovina, Triassic magmatic rocks are associated with platform carbonate sediments and also occur frequently within Palaeozoic–Triassic allochthonous series (mountains of Central Bosnia, Sana–Una Palaeozoic complex, south- east Bosnia near Čajniče, Foča, Tjentište and Kalinovik – Fig. 1). Keywords: alteration; area; basalt; chlorite; dinarides; elements; fig; magmatism; plagioclase; rocks; samples; triassic; volcanic
• Alluvial Architecture and Fluvial Cycles in Quaternary Deposits in a Continental Interior Basin, E Hungary by Juhasz, Györgyi; Müller, Pal; Toth-Makk, Agnes (2010) - In the context of carbonate systems, not fluvial cycles, STRASSER et al. (1999) show a hierarchical stacking of depositional sequences, and define small-scale, medium-scale and large-scale sequences. Juhasz et al.indd Alluvial Architecture and Fluvial Cycles in Quaternary Deposits in a Continental Interior Basin, E Hungary Györgyi JUHÁSZ, Pál MÜLLER and Ágnes TÓTH-MAKK 1. Keywords: area; basin; channel; cycles; deposits; facies; fig; floodplain; fluvial; körös; quaternary; sandy; scale; sequence; succession; zone
• Diagenesis of Upper Cretaceous Rudist Bivalves, Abu Roash Area, Egypt: A Petrographic Study by Mansour, Ahmed Sadek M. (2010) - Similar diagenetic alterations of rudist shells are reported by AL-AASM & VEIZER (1986a) and WOO et al. (1993). EL-SABBAGH, A.M. & EL-HEDENY, M.M. (2003): Upper Turonian Radiolitidae (rudist bivalves) from the Acta- eonella series, El-Hassana dome, Abu Roash, Egypt.– Egyptian J. Paleontology (in press). Keywords: abu; area; calcite; carbonate; cement; cretaceous; crystals; diagenesis; equant; meteoric; rudist; shells; silica; silicification
• Impact of Geomorphological Variables in Weighing the Lithological Influence on Geochemical Composition of Stream and Overbank Sediments: A Regression Model for the Žumberak Area (NW Croatia) by Peh, Zoran; Miko, Slobodan (2010) - The regression results acquired in this admittedly restricted study indicate that the geochemical signature of drainage basin sediments grossly reflects their sourc- ing from the basin parent lithology, but the patterns of compositional variation are not easy to assess as these depend on a variety of processes. As a contrast, with stream sediments not only a smaller number of elements are better explained by the linear approach but also the positive R2 difference is generally much less (with the exception of Ni and Cu). Keywords: area; basin; channel; drainage; elements; influence; kupa; linear; lithology; material; miko; overbank; regression; rocks; sediment; stream; variables; žumberak
• Palaeogeographic Variability and Depositional Environments of the Upper Jurassic Carbonate Rocks of Velika Kapela Mt. (Gorski Kotar Area, Adriatic Carbonate Platform, Croatia) by Velić, Ivo; Tišljar, Josip; Vlahović, Igor; Velić, Josipa; Koch, Georg; Matičec, Dubravko (2010) - 1 Location map of the study area with the distribution of Upper Jurassic deposits of different palaeoenvironments. In the neighbour- ing areas of NW Gorski Kotar, NW Lika and Velebit, as well as in the Velika Kapela Mt. and area NE of it, Upper Jurassic deposits are characterised by differ- ent, but exclusively shallow-marine facies, deposited within shallow lagoons, low-energy shallow subtidal to peritidal environments. Keywords: area; carbonate; cherts; deposits; environments; fig; jurassic; kapela; limestones; lithofacies; marine; platform; shallow; trough; velika; velić; zagreb
• Carbonate Platform Megafacies of the Jurassic and Cretaceous Deposits of the Karst Dinarides by Tišljar, Josip; Vlahović, Igor; Velić, Ivo; Sokač, Branko (2010) - Carbonate platform deposits of the Karst Dinarides are, besides their significant thickness (4500–8000 m, 6000 m in average), characterised by frequent lateral and vertical alternations of different facies, mostly associated with shallow marine environments. This megafacies prevails in Velika Kapela Mt. and in the Senj–Ogulin profile (locality Fig. 2 Correlation of Jurassic and Cretaceous platform carbonate megafacies from the Senj–Ogulin profile (modified after MATIČEC et al., 1997), Triassic, Jurassic, Cretaceous and Palaeogene carbonates of northern margin of the carbonate platform in the Karlovac–Duga Resa area (modified after BUKOVAC et al., 1974; DRAGIČEVIĆ & VELIĆ, 1994, 2002), and Cretaceous–Palaeogene carbonates of northern margin of the carbonate platform in the Donji Bešpelj area, Bosnia and Herzegovina (modified after DRAGIČEVIĆ, 1987; DRAGIČEVIĆ & VELIĆ, 1994). Keywords: adriatic; area; bauxites; carbonate; carbonate platform; central; cretaceous; croatia; deposits; diagenetic; dinarides; dolomites; environments; et al; geol; island; istria; jurassic; limestones; ljubljana; localities; locality; megafacies; middle; peritidal; platform; platform megafacies; shallow; slovenia; sokač; tišljar; upper; velić; vlahović; water; western; zagreb; zavod
• The Karst Dinarides are Composed of Relics of a Single Mesozoic Platform: Facts and Consequences by Vlahović, Igor; Tišljar, Josip; Velić, Ivo; Matičec, Dubravko (2010) - Undoubtedly during this period the studied area represented only a part of a larger shallow water 176 Geologia Croatica 55/2 177Vlahović, Tišljar, Velić & Matičec: The Karst Dinarides are Composed of Relics of... carbonate platform, being connected, e.g. with the area of the future Apulian and Apenninic platforms. However, carbonate platforms which are located along the SW coast of the Adriatic Sea, and which have the same foundation as the platform stud- ied in this paper since they were formed on the Adria Microplate after its disintegration in the Late Lias, have their specific names – Apulian and Apenninic Carbonate Platforms. Keywords: adriatic; area; carbonate; carbonate platform; cretaceous; deposits; dinarides; et al; geol; karst; marine; platform; tišljar; velić
• The Northeastern Margin of the Adriatic Carbonate Platform by Dragičević, Ivan; Velić, Ivo (2010) - Strojice The column was measured NW of Kupres (Fig. 1, location 22), where an exposed sequence (85 m thick) consists of carbonates of platform margin and carbonate clastic slope deposits occurs towards one of the intra- platform troughs in the general area of the NE margin of the AdCP (Fig. 23). They are overlain by slope limestones of the Late Lias: mud-supported mostly fossiliferous wackestones with lithoclasts of platform limestones, rarely containing ooids, Involutina liassica (JONES), lagenids, nodosarids and other organ- isms of the slope biotope. Keywords: 55/2; adriatic; age; area; basinal; beograd; bosnia; carbonate platform; carbonates; cenomanian; column; cretaceous; croatica; deposits; et al; facies; fig; geološka; jurassic; karta; limestones; maastrichtian; map; marine; middle; osnovna; platform margin; platform slope; reef; savezni; sediments; sfrj; shallow; sheet; slope; velić; zavod
• A Factor Model of the Relationship between Stream Sediment Geochemistry and Adjacent Drainage Basin Lithology, Medvednica Mt., Croatia by Halamić, Josip; Peh, Zoran; Bukovec, Dragan; Miko, Slobodan; Galović, Lidija (2001) - ZAGREB 2001 Key words: Stream sediment, Lithology, Drainage basins, Geochemical composition, Factor analysis, Medvednica Mt., Croatia. Factor analysis The exploratory factor analysis is a powerful mathemat- ical and statistical tool in handling a great number of numerical data. Keywords: area; elements; factor; fig; geochemical; lithology; medvednica; mesozoic; model; relationship; rocks; sediment; stream; variables
• Geochemical Comparison of Stream and Overbank Sediments: A Case Study from the Žumberak Region, Croatia by Peh, Zoran; Miko, Slobodan (2010) - Zn, Pb, Cu and As distribution patterns in overbank and medium- order steam sediment samples: their use in exploration and environmental geochemistry.- J. Geochem. Only the carbonate material seems to be deplet- ed in overbank sediment samples. Keywords: analysis; area; carbonate; discriminant; drainage; elements; kupa; material; media; overbank; sample; sampling; sediment; stream
• Shoreline Cross-bedded Biocalcarenites (Middle Miocene) in the Podvrsko-Snjegavic Area, Mt. Psunj, and their Petroleum Significance (Pozega Subdepression - Eastern Croatia) by Velić, Josipa; Tišljar, Josip; Dragičević, Ivan; Blašković, Ivan (2010) - ZAGREB 2000 Key words: Cross-bedded biocalcarenites, Shoreline deposits, Subaqueous dune, Petroleum and gas re- servoir sandstone, Synsedimentary tectonics, Bade- nian, Poæega subdepression, Pannonian basin, East- ern Croatia. Cross-bedded biocalcarenites with the landward 292 Geologia Croatica 53/2 inclined foresets were not found in the Podvrπko- © n j e- gaviÊ area. Keywords: area; badenian; biocalcarenite; bodies; cross; detritus; fig; foresets; miocene; psunj; rocks; sea; sediments; sets; siliciclastic
• Seismotectonically Active Zones in the Dinarides by Kuk, Vlado; Prelogović, Eduard; Dragičević, Ivan (2010) - The frequency of earthquake occurrence and con- centrations of their foci enable definition of the spatial position of seismotectonic zones. The following observations are the most important: - stacking of a number of seismotectonic zones at vari- ous depths implies the greater activity of the area; - mildly inclined zones, and especially the length of the 30 km of the zone correlated with the Mosor - Bioko- vo fault depict the reverse-overthrust displacements; - the strongly expressed bending of the zone correlated with the Mosor - Biokovo fault, formation of the branching fault and the vertical faults around the Imotsko polje point out to the possibility of rotation of structural units, and to the oblique spatial move- ments in respect of their strike, as well as to the hori- zontal displacement on the vertical faults. 3.6. Keywords: activity; adriatic; area; earthquake; fault; mcs; section; zones
• Quaternary Deposits as the Hydrogeological System of Eastern Slavonia by Bačani, Andrea; Šparica, Marko; Velić, Josipa (2010) - i t s cover large areas in the Brodsko Posavlje region and in eastern Posavina. The eastern Slavonia area was then covered by shallow lakes and swamps and the neighbouring Bosnian and Slavonian mountains were land areas exposed to strong denudation. Keywords: area; beograd; drava; eastern; fig; geol; plateau; sava; sediments; slavonia; vinkovci; vukovar; zagreb; zavod; zones
• Tectonics of Part of the Vinodol Valley Within the Model of the Continental Crust Subduction by Blašković, Ivan (2010) - Ti pokreti su shvaÊeni kao svojevrsna najava dezintegracije karbonatne platforme u ovom dijelu Dinarida, a naπli su odraza u formi- ranju blagih antiklinalnih Ona je u reversnom rasjednom kontaktu s paleo- genskim fliπom Vinodola. Keywords: action; akcije; anticlinal; area; badanj; bla; breëa; carbonate; characteristics; complex; contact; continental; croatica; crust; deposits; dijelom; dijelu; dio; dip; direction; doline; eastern; fault; fig; fliπnih; flysch; foraminiferskih; geologia; hanging; ili; izmeu; kao; kovi∆; kretanja; krila; limestones; model; movement; nagiba; naslaga; north; odnosno; otpora; padine; palaeogene; paleogenskih; plane; pliocene; plohe; podvlaëenja; position; prema; rasjeda; rasjedne; reverse; sediments; sjeveroistoku; sjeveroistoëne; slojeva; sopalj; south; stijena; structures; struktura; subduction; subdukcije; tectonics; uglavnom; uplift; valley; vapnenaca; vapnenci; vinodol; vinodol valley; wall; western; zone
• A Middle Jurassic Radiolarite-Clastic Succession from the Medvednica Mt. (NW Croatia) by Halamić, Josip; Goričan, Špela; Slovenec, Damir; Kolar-Jurkovšek, Tea (2010) - Rock samples were milled into powder and homoge- nized in an agate mill. Rock samples, residues and SEM negatives are stored in the col- lection of the second author. Keywords: area; cherts; elements; fig; figs; gori»an; grey; halami∆; jurassic; kozur; matrix; medvednica; middle; poljanica; quartz; radiolarian; radiolarites; rocks; samples; shales; succession; triassic
• Tectonic Interrelation of the Dinarides and the Southern Alps by Herak, Milan (2010) - MESOZOIC DEPOSITS WITH PELAGIC INFLUENCES The outcrops of Late Triassic pelagic deposits are encircled either by platform or by oceanic facies from which they can be distinguished: from the platform for- mations by the type of sediments (platy limestones, radiolarites, etc.), and from the oceanic formations by a lack of a magmatic-sedimentary complex with ultra- mafics and mafic intrusives. Epiadriaticum (pelagic deposits and clastics with pelagic components); 8) Adriaticum; 9) ? Keywords: alps; area; carbonate; deposits; dinarides; elements; geol; medvednica; nappe; oceanic; outcrops; pelagic; platform; rocks; triassic; zagreb; zone
• Professor Herak's Contribution to Triassic Stratigraphy by Koch, Georg; Grgasović, Tonći (2010) - The widespread carbonate successions of the Zumberak Mountain were also proven to be Late Triassic in age (HERAK et aI., 1965). In the same area, HERAK (1960c) identified the disconti nuity between the Permian and the Triassic, proved the Middle Trias­ sic, and complcted thc interpretation of the discontinu­ it y bctween the Middle and Late Triassic. Keywords: algae; area; croatia; dasyclad; deposits; der; des; dinarides; geologija; herak; nas; podrucju; professor; research; stratigraphy; thc; triassic; trijasa; vjesnik; von; work; zagreb
• Professor Herak's Contribution to Karst Geology and Hydrogeology by Bahun, Stjepan; Biondić, Božidar (2010) - Thi s bulky and enduring project was given to Herak who, after hi s long term effective and globally recog­ nised karst research, became an outstanding connois­ seur of karst geology. The paper published in 1977 entitled Tecto-genetic approach to the classification of karst terrains (Tekto­ genet ski pristup klas ifikaeiji krskih terena) represented the condensation o[ all Herak 's knowledge. Keywords: approach; area; geology; herak; hydrogeology; karst; reservoir; river; zagreb
• Triassic Deposits of Hrvatsko Zagorje by Šimunić, Antun; Šimunić, Alka (2010) - The most detailed geological cross section through Upper Triassic deposits in Northwestern Croatia was discovered in a quarry ncar Podsused, in the northwest­ ern part of Medvednica Ml., but later, unfortunately, completely destroyed due to mining. vednica Mt., where Triassic rocks occur in a much mo­ re complicated form, most ly as the remnants of over­ thrusts (SIKIC et aI., 1979). Keywords: anisian; arc; area; carbonate; clastics; deposits; dolomites; geological; gora; grey; herak; hrvatsko; ivanscica; limestones; middle; mountains; ravna; rocks; sediments; simunic; triassic; zagorje; zagreb
• Tectonic Structures Along the Periadriatic Lineament in Slovenia by Mioč, Pero (2010) - [997 Tectonic Structures Along the Periadriatic Lineament in Slovenia Pero MIOC Key words: Pcriadriatic lineament , Karavankc, Tecto­ nic st ruc tu re, Zone of Periadriatic lineament, ol1h­ ern Karavankc thrust, Velunja thnlst, Olsev3-Kosuta thrust, Southern Karavanke thrust. The lec(Qnic contact of the Olseva-Kosuw unit with (he Southern Karavanke unit Oil the southern slopes ot Olseva. Keywords: alps; area; basin; beds; belt; eastern; fig; geol; granite; karavanke; limestones; lineament; mioc; mountains; northern; parts; periadriatic; rocks; sediments; slovenia; southern; tectonic; thrust; triassic; unit; zone
• Stratigraphy and Tectonic Relationships Along the Senj - Ogulin Profile (Velika Kapela Mt., Croatia) by Matičec, Dubravko; Vlahović, Igor; Fuček, Ladislav; Oštrić, Nenad; Velić, Ivo (2010) - With the exception of a narrow zone of Neocomian deposits (Lithostratigraphic Unit I) out cropping in the men­ ti oned tectonic zone, thi s Uni t is composed of the almo­ st com plete ly dol omi ti zed Tithonian deposits (Lithos­ tratig raphi c Unit I-I). The complete thickness of Lithostratigraphic Unit E is approximately 400 ITI. Keywords: age; area; beds; deposits; fault; figs; profile; strike; structure; tectonic; thi; thickness; tithonian; unit
• Glaciation Traces in the Area of the Risnjak Mountain Massif by Bognar, Andrija; Prugovečki, Ivančica (2010) - OF THE RISNJAK MOUNTAIN MASSIF T he Risnjak mountain massif represents a submor­ phological regional un it of the mesogeomorphoiogicai regio n of the nort h-weste rn part of Gorski KOlar. The Risnjak mountain massif is div ided into a series o f geomorphological microregions: the mountain range o fV eliki Risnjak ( 1,528 m) and Mali Risnjak ( 1,448 m); the mounta in range of Janjicarski veh (1,3 14 m), Vc liki Bukovac ( 1,266 m) a nd Mali Bukovae (1 ,263 m ); the mOllntai n rangc or Velika !iija (l,172 m) and Mala Sija ( 1,149 m); the Ostra mountain range (1,221 m) , the Segi nscek mountain range (1,145 m), the uvala Lazac ( 1,060 m), a seri es o r uvalas at Gasparae (940 m) - Seg ine (950 m), the lI va la Lividraga (918 m) and th e plain of the Suha Retina river. Keywords: area; blocks; erosion; fig; forms; glacial; glaciation; glaciers; height; line; lividraga; mali; massif; moraine; mountain; pleistocene; range; risnjak; sneznik; snow; temperature; terminal; today; worm; zagreb
• Hydrogeological Exploration of the Rječina River Spring in the Dinaric Karst by Dukarić, Franjo; Kuhta, Mladen; Biondić, Ranko (2010) - The Rjecina spring is an int ermittent karst spring reaching a maximum di scharge rate of 120 m3/s (annual average about 8 m3/s). I 1110311996 rccordcd in thc shal low pans of aquifer (Fig. 9), which is the normal situation in spring zones. Keywords: aquifer; area; carbonate; catchment; catchment area; exploration; fig; grobnicko; groundwater; hydrogeological; karst; north; polje; river; rjecina; rjecina spring; rocks; seasons; spring; summer; water; zone
• Hydrogeological Evaluation of Water Retaining Properties of the Kosinj Reservoir (Lika, Croatia) by Pavičić, Ante (2010) - PA VICI<': (1995) in hi s PhD Lhesis described the hydrogeological condiLions for the construction of water reservoirs in the karst of the VclebiL hinLeriand , where he also sLudied the area around Kosinj . Legend: I) grou nd water above the Lika river stage: 2) Jehu deposits impenneablc as a unit; 3) rclative ly uplifled tcctonic block; 4) terrain under a highcr influence of clay deposi ts; 5) low groundwatcr under Lika river: 6) faul l; 7) major karst spri ng. pennanent; 8) major karst spring. Keywords: area; bakovac; barrier; beds; conditions; fault; fig; flow; fritz; groundwater; karst; karstification; kosinj; kosinj reservoir; level; lika; lika river; polje; reservoir; river; rocks; spring; studies; terrain; thc; valley; velebit; water; zone
• Frequency Distribution Curves as an Indicator of Evolutionary Trends in Geomorphological Systems: A Case Study from the Northwestern Part of Hrvatsko Zagorje (Croatia) by Peh, Zoran (2010) - Geomorphi c thresholds and complex response of drainage system s.- In: MORI­ SA WA, M. (cd.): Another group of geomorphological processes is distinguished by a normal frequency distribution curve of lluctuations, indicating structural stabilit y of the per­ taining subsystems, which is a consequence of their ability to maintain thei r structural attributes in the exist­ ing regime of external forces. Keywords: area; basin; curves; dissection; distribution; drainage; energy; equilibrium; fig; frequency; geomorphological; landforms; landscape; new; order; processes; slope; study; system
• The Petroleum Fiscal Regime and Oil Company Status by Vlašić, Boro; Lipovac, Hrvoje (2010) - The present status of the oil market strongly influences the potential entrance of foreign investors into oil exploration in Croatia. The negotiations arc held between an oil compa ny and the govern ment representativc (government agency, national oil company and some­ times ministry for natural resou rces). Keywords: agreements; area; company; country; croatia; exploration; law; mineral; oil; production; profit; reserves; state; thc
• A Geodetic-Gravimetric Method for Better Modelling of Geological Structures in the Test Area of Croatia by Čolić, Krešimir; Bašić, Tomislav; Pribičević, Boško; Medak, Damir (2010) - Init ial digi ta l density model of the surrace Earth's core masses in the test area Slovenia and surround­ ing palt of Croatia for the regional uses in physical geodesy.- Geodetski lis t. 46/3, 263-281, Zagreb. Topographic correction from 3D density model (i ll 10-5 ms·2) : b) deflections of vertical rrOTll 3D : 05 00 density model (in arcscc) . Keywords: area; data; density; depths; earth; fig; model; rs7; surface; vertical
• Expansion of the Old Oil Field of Bunjani on the Basis of Geological Reinterpretation by Filipović, Niko (2010) - Th e rese rvoir data summary of the Bunjani oi l field is shown in Table I. Reservoir l+1I: 5. CONCLUSION Based on the geological reinterpretation carried out on the old Bunjani oi l field, lhe following conclusions may be drawn: I. Keywords: area; beds; bunjani; data; extension; fault; field; fig; marl; new; oil; production; reinterpretation; reservoir; rocks; sandstones; water; wells
• Selection of Exploration Strategy by Kolundžić, Stevo (2010) - 3 Forecasts of oi l production and revenue: a) oil production; b) cash now. World oil exploration, paI1icularly drilling, has been conside rably red uccd si nce 1986, until the present. Keywords: area; costs; croatia; efficiency; exploration; fields; gas; increase; number; oil; price; production; reserves; table; world; year
• Geothermal Energy Resources in the Republic of Croatia - Overpressured Zone by Mesić, Ivan; Krištofek, Branko; Babić, Tamara (2010) - Th e second type or this reservoir is hot water. Hydrothermal convection resource (heat carried upward by water or steam convection): a) vapor dominated with temperatures around 240°C. b) hot water dominated wi th tempera tures from 350°C to less than 90°C. 2. Keywords: area; geothermal; sequences; temperature; water; zone
• Geological Characteristics of the Oil Fields in the Sloven ian Part of the Pannonian Basin by Mioč, Pero; Žnidarčič, Miro (2010) - On [his basis, and as a consequence of recent results of oil geo logical investi ­ gat ions, lhe li thostratigraphic description of lhe Neogene beds of Ihis part of the Pannonian basin is presented , together wilh occurrences or source rocks in the given strat igraphic horizons, as well as the struc­ tural charactcristics or thc tcrrilOry. Beds of marls, clayey marls and clays occur in individual parts of these stra tigraphic units , and they can form favourable traps. Keywords: antiform; area; basement; beds; depression; fields; gas; mioc; mura; murska; neogene; oil; pannonian; reservoir; rocks; sobota; units
• Hydrocarbon Reserves - Estimation, Classification and Importance in Evaluation of Exploration Projects by Nadjaković, Zvonimir; Sečen, Josip; Bauk, Antun (2010) - ZAGREB 1996 I NCl'iew paper Hydrocarbon Reserves - Estimation, Classification and Importance in Evaluation of Exploration Projects Zvonimir NADJAKOVIC, Josip SECEN and Antun BAUK PROCEEDINGS Key words: Hydrocarbon reserves, Classification of reserves, Evaluation of exploration projects. This means that th e process of exploring, discovering and putting into pro­ duction new reserves is continuous, but under consider­ ably more difficult technical and economi c condi tions, as is constantly reite rated by the leading people of big oil compan ies . Keywords: approach; arc; area; company; costs; evaluation; exploration; hydrocarbons; market; oil; petroleum; production; recoverable; reserves; value; world
• The gully of Potovošća on the island of Krk – The effects of a short-term rainfall event by Faivre, Sanja; Pahernik, Mladen; Maradin, Mladen (2011) - Rapid changes of the Potovošća beach occur particularly in stormy weather. The Potovošća beach is embayed and 121 m long. Keywords: area; basin; beach; beaches; data; drainage; event; gully; intensity; krk; level; potovošća; precipitation; rainfall; runoff; sea; stations; term; time
• gc-400 by None (None) - Osnovna geoloska karla SFRJ I: 100000, lisl l lirska Bistrica.- Zvczni gcoloski zavod, Beograd. Il oweve r, de lajieci investigat ions have shown that Ih is area is built lip predominantl y o f va rious types of fo lds Ihal are onl y slight ly displaced along reverse faults (Fig. Keywords: area; northeast
• gc-433 by None (None) - \Vithout excluding some su baerial erosion, or possibly somewha t condensed deposition, we consider that in the discussed areas of Istria, the major part of thc Cretaceous deposits was not deposited, as a consequence of thc relatively mild, but during the Cretaceous continuously present synscdi ­ men tary tectonics. Lower Cretaceous deposits: 2) Cenomanian deposits: 3) Turonian ­ Santonian deposits: 4) Palaeogene Foraminiferal limestones and flysch deposits: 5) Keywords: age; albian; area; carbonate; cenomanian; cretaceous; deposits; eocene; fig; foraminiferal; geol; hauterivian; istria; land; late; limestones; orientation; palaeogene; polsak; thc; zagreb
• gc-452 by None (None) - Type I includes the si lty-grav elly sands of Unit III , gravell y­ sands (llld snndy-silty gravels of Unit II and gravelly­ sandy interbeds of Unit 1. Unit II Keywords: age; area; bp-4; brown; carbonate; changes; chlorite; clay; clayey; colour; coloured; composition; concretions; core; deposits; drill; environment; fig; figs; gravels; grey; iii; ing; lake; loess; log; material; middle; mineral; pebbles; pleistocene; presence; processes; quaternary; red; results; rocks; sand; sediments; silt; soil; thickness; unit; unit iii; water; yellowish; zagreb
• gc-468 by None (None) - This is demonstrated by the similarity of the ground morphology with extension of the border between the Promina sedi ments and Upper Permian deposits in the area of Badanj, Umljanović and Markovac, and particularly the composition of basal Promina conglomerates east of the Krasići hamlet at Drniš Geologia Croatica 45 (SAKAĆ, 1970). 103 IVANOVIĆ et al. (1971) state that the porous carbonate breccias near Orlić (Kosovo polje) are located between red clastics and Lower Triassic deposits, and conclude that they most probably belong to the Upper Permian - Lower Triassic transition, and they could be coastal material formed in the Upper Perm ian along the borderline of emergent surfaces and the evapori tic basin, in a zone of alternative flooding and drainage. Keywords: age; area; bosnia; breccias; carbonate; clastics; complex; deposits; der; dolomites; evaporites; geol; geological; grey; gypsum; investigations; klaus; kosovo; lika; limestones; middle; naslaga; occurrences; permian; places; polje; relations; rocks; sediments; sinj; site; suhač; tectonic; triassic; upper; valley; zagreb
• Factor Model of the Geomorphological System of a Part of Northwestern Croatia by Peh, Zoran (2010) - Therefore, there is no need for detailed discussion on the aims and purposes of factor analysis and characteristics of factor model. ZAGREB 1992 UDC 551.4:04 (497.13): 519.24 Sciefintic paper Factor Model of the Geomorphological System of a Part of Northwestern Croatia Zoran PEH Key words: factor model, drainage basin system, re­ sistant geological framework, driving forces, geomorphic processes, geological structure, lithology The method of factor analysis (R-mode) is applied as a tool in the system approach to the investigation of a selected geomorphologi­ cal region in the Northwestem Croatia. Keywords: analysis; area; basin; drainage; factor; factor model; forces; geol; geološki; gora; landscape; lithologic; model; morphometric; processes; relationship; rock; sandstones; shales; slope; study; system; valley; variables; zagreb
• Bio- and Sequence Stratigraphy of Upper Cretaceous – Palaeogene rocks, East Bahariya Concession, Western Desert, Egypt by Mahsoub, Mohamed; Abulnasr, Radwan; Boukhary, Mohamed; Faris, Mahmoud; Abd El Aal, Mohamed (2012) - Abu Roash Formation The type locality of the Abu Roash Formation outcrops to the north of the Pyramids of Giza (30° 2' 44.59“N and 31°14' 24.71“E). displays discon- tinuous, moderate to low amplitude refl ectors. Keywords: abu; age; area; bahariya; cretaceous; croatica; desert; east; ectors; egypt; eocene; formation; karama; limestone; marine; refl; roash; sediments; sequence; shale; stratigraphy; systems; tract
• Sedimentary evolution of an inner foreland basin margin: Paleogene Promina Beds of the type area, Mt. Promina (Dinarides, Croatia) by Zupanič, Jožica; Babić, Ljubomir (2011) - Lithostratigraphic names would be as follows: Kalun Conglomerate (U1; Basal alluvium) Varoš Formation (U2; Lower lacustrine unit) Knezovi Conglomerate (U3; Lagoon to alluvium) Počivalica Formation (U4; Middle lacustrine unit) Previje Formation (U5; Shelf/delta alternation) Bukovac Limestone (U5A; Fossil-rich Limestone) Unnamed formation (U6; Upper lacustrine unit) Čavnovka Conglomerate (U7; Terminal alluvium) 2. ALLOSTRATIGRAPHY Thus, the names for the units in MtP, which would constitute the Promina Allogroup, may be as follows: Kalun Conglomerate Alloformation (U1; Basal alluvium) Varoš Alloformation (U2; Lower lacustrine unit) Knezovi Conglomerate Alloformation (U3; Lagoon to allu- vium) Počivalica Alloformation (U4; Middle lacustrine unit) Previje Alloformation (U5; Shelf/delta alternation) Bukovac Limestone Alloformation (U5A; Fossil-rich Lime- stone) Unnamed alloformation (U6; Upper lacustrine unit) Čavnovka Conglomerate Alloformation (U7; Terminal allu- vium) 3. SUBDIVISION AND NAMING OF UNITS OF THE PROMINA BEDS: A COMPARISON The lithostratigraphic subdivision may be useful, as generally confi rmed by its widespread use. Keywords: alluvial; area; babić; basin; calcarenites; conglomerates; croatica; cycle; delta; evolution; fig; foreland; marine; mtp; promina; sediment; sequence; shelf; unit; zupanič
• Origin and distribution of surface sediments in the Grgur Channel, Adriatic Sea, Croatia by Pikelj, Kristina; Žigić, Višnja; Juračić, Mladen (2009) - Grgur Channel coasts (Fig. 2) are exposed to marine erosion (BENAC, 1992), especially due to waves generated by the Jugo. In: CUSHMAN-ROISIN, M. B. et al. (eds): Physical Oceanography of the Adriatic Sea, Klu- wer, Dordrecht, 189–214. PIGORINI, B. (1968): Sources and dispersion of recent sediments of the Adriatic Sea.– Mar. Geol., 6/3, 187–229. SURIĆ, M., JURAČIĆ, M., HORVATINČIĆ, N. & KRAJCAR BRONIĆ, I. (2005): Late Pleistocene–Holocene sea-level rise and the pat- tern of coastal karst inundation: records from submerged speleo- themes along the Eastern Adriatic Coast (Croatia).– Keywords: adriatic; area; channel; fig; fraction; grain; gravel; gravelly; grgur; grgur channel; kvarner; sea; seabed; sediments
• A complex landslide in the Rječina Valley: results of monitoring 1998-2010 by Benac, Čedomir; Dugonjić, Sanja; Vivoda, Martina; Oštrić, Maja; Arbanas, Željko (2011) - benac.indd 239 � AB STRA CT Results of landslide monitoring undertaken between 1998–2010 on the north-eastern slope of the central part of Rječina Valley in front of Grohovo village (north-eastern coastal part of Adriatic Sea, Croatia) are presented. A major part of the monitoring equipment will be installed in the active landslide zone on the north-eastern Figure 2: A view of investigated zone of the Rječina Valley (photo: ARBANAS, Ž.) Benac et al.: Keywords: area; benac; landslide; limestone; mass; monitoring; movements; rječina; rječina valley; slope; valley; ysch
• New paleomagnetic results from imbricated Adria: Ist Island and related areas by Marton, Emo; Moro, Alan (2009) - Table 2: Oveall mean palaeomagnetic directions for Cenomanian–Early Senonian localities, before and after tilt corrections with statistical parameters and palaeomagnetic poles calculated from the tilt-corrected directions for Ist island and related areas, for stable Istria (the fi rst version comprises the Cenomanian and Early Senonian localities, the second also Turonian localities) and for the Kvarner islands. Transact., 39, 4, 227–232. MÁRTON, E., PAVELIĆ, D., TOMLJENOVIĆ, B., PAMIĆ, J. & MÁR- TON, P. (1999): First palaeomagnetic results on Tertiary rocks from the Slavonian mountains in the southern Pannonian basin, Croatia.– Geol. Keywords: adriatic; area; directions; fig; islands; márton; senonian
• Engineering properties of marine sediments in Mali Ston Bay (Croatia) based on “Mainland-Pelješac” bridge investigations by Buljan, Renato; Pollak, Davor; Gulam, Vlatko (2012) - The exploration works also documented sediments with several characteristic depositional environments, character- ized by specifi c engineering properties in particular those re- lated to overburden depth: unit A – alternately marine and brackish environment with low overburden – very soft to soft sediment; unit B – shallow marine with low and rare higher energy periods, with overburden of several tens of metres – soft to fi rm sediment; unit C – deeper and very low energy marine deposition environment, with overburden of more tens of metres up to hundred metres – fi rm sediment. Based on 7 profi les with a total depth of 457 m. Figure 13: Comparison of the consistency index (IC) and cone penetration resistance (qc) in particular engineering geological units. Keywords: adriatic; area; bridge; carbonate; engineering; figure; geological; marine; material; pelješac; properties; samples; sea; sediments; unit
• Geothermal properties of the northern part of the island of Rab by Kovačić, Miron (2013) - doi: 10.1007/s10347-007-0120-6 PRELOVŠEK, P. & URAN, B. (1984): Generalised hot wire method for thermal conductivity measurements.– J. Phys. The intention was to analyse 15 samples of rock from Table 1: Statistical analysis of the results of thermal parameters measurement (λ (k) – coefficient of thermal conductivity, cρ – volumetric heat capacity, a – thermal diffusivity, Min.- lowest measured value, Max. - highest measured value, Mean – mean value of a thermal parameter) Sample name Sample description GEOTHERMAL PARAMETERS l (k) (Wm–1K–1) cr (Jm–3K–1) Keywords: area; conductivity; cretaceous; geothermal; heat; limestone; mean; samples; values; water
• Co-occurrence of Sinuspores sinuatus (Artüz) Ravn 1986 with established palynological markers indicating younger strata: AK-1X well section (Pennsylvanian, Zonguldak Basin, NW Turkey) and the correlation to the stratigraphic system by Stolle, Ellen (2012) - The relevant foraminiferal event (from GRADSTEIN et al., 2004) has been included to chart C) for overview and comparison with charts A) and B) as it represents ‘age control’ for the palynological events. The European regional stages probably have been adapted to the ‘Atokan’ accord- ing to correlations of GRADSTEIN et al. (2004) (compare to C). Keywords: ak-1x; area; carboniferous; et al; fig; iowa; range; section; sinuatus; sinuspores; turkey; westphalian; zonguldak
• Assessment of aquifer intrinsic vulnerability by the SINTACS method by Kapelj, Sanja; Loborec, Jelena; Kapelj, Janislav (2013) - POLEMIO, M., CASARANO, D. & LIMONI, P.P. (2009): Karstic aq- uifer vulnerability assessment methods and results at a test site (Apulia, Southern Italy).− Nat. UHAN, J., PEZDIČ, J. & CIVITA, M. (2008): Assessing groundwater vulnerability by SINTACS method in the Lower Savinja Valley, Slovenia.− RMZ-Materials and Geoenvironment, 55/3, 363−376. Keywords: aquifer; area; assessment; catchment; density; groundwater; jadro; method; parameter; rocks; sintacs; vulnerability; žrnovnica
• Simulation of Groundwater Mound Resulting from Proposed Artificial Recharge of Treated Sewage Effluent Case study – Gaza waste water treatment plant, Palestine by Aish, Adnan Mousa (2010) - Keywords: Artifi cial recharge, Groundwater modeling, Groundwater mounding Simulation of groundwater mound resulting from proposed artifi cial recharge of treated sewage effl uent case study – Gaza waste water treatment plant, Palestine � Adnan M. Aish Department of Geology, Faculty of Science, Al Azhar University – Gaza, P.O. Box 1277 The average of the monthly maximum temperature ranges between 17.6 C° for January to 29.4 C° Adnan M. Aish: Simulation of groundwater mound resulting from proposed artifi cial recharge of treated sewage effl uent case study... Keywords: aquifer; area; gaza; groundwater; infi; level; ltration; mound; recharge; strip; study
• The geology of the Camerano area through the reconstruction of sedimentary sequences of the urban caves by Bizzarri, Roberto; Baldanza, Angela; Luccioni, Irene; Recanatini, Alberto (2013) - The main structure of the Periadritic Basin is the result of at least three different tectonic phases, that took place from the Miocene to recent times (CALAMITA et al., 1991; ORI et al., 1991; CELLO et al., 2009). Calcareous nannofossils - The Calcareous nannofossil analysis has been carried out in clay deposits, as they are to- tally missing in sand horizons. Keywords: area; basin; beds; camerano; cantalamessa; centamore; clay; couplets; croatica; deposits; doi; et al; fig; flow; geol; grotta; matrix; pleistocene; sand; section; sedimentary
• Distribution and bioavailability of manganese in soil in the vicinity of the „Bužim“ abandoned mine by Redžić, Safeta; Sijarić, Galiba; Muhić-Šarac, Tidža; Pehić, Ekrem; Hrnjica, Damir (2014) - It was determined that chemical properties of soil considerably affect the distribution of heavy metals within different soil fractions. Methodology for the sequential extraction of manganese from the soil The defined steps and reagents used in the process of sequential extraction are shown in Table 1. Extracts from different soil fractions were separated by centrifugation at a speed of 3000 rpm for a period of 30 mi- nutes, collected in polyethylene bottles and stored at 4 °c until analysis according to the references (AGNIESZKA & wITOLD, 2004; MING et al., 2008; SILVEIRA et al., 2006; KAZI et al., 2005; PUEYO et al., 2008; DAVIDSON et al., 2006; JOSE et al., 2006; KAASALAINEN & YLI-HALLA, 2003; ROUHOLLAH & FARZANEH, 2010). Keywords: 1st; area; et al; extraction; fraction; horizon; iso; locations; manganese; percentage; polje; profile; samples; soil; total
• Conceptual model for groundwater status and risk assessment - case study of the Zagreb aquifer system by Nakić, Zoran; Ružičić, Stanko; Posavec, Kristijan; Mileusnić, Marta; Parlov, Jelena; Bačani, Andrea; Durn, Goran (2012) - the model is divided into two parts: a) Global Conceptual Model (GCM), which provides an insight into the processes at the level of groundwater system and b) Local Conceptual Model (LCM), which supports parameterization of the groundwater system through small scale experiments conducted at two sites: Ko- snica, which provides an insight into the behaviour of con- taminants in the unsaturated zone and Stara Loza, which pro vides an insight into small scale heterogeneity. Taking into consideration knowledge gaps in the under- standing of groundwater systems, a coherent approach to as- sess a risk for a wide range of source-pathways-receptor re- lationships at different scales is applied by dividing the con ceptual model in two parts: a) Global Conceptual Model (GCM), which gives an insight into the processes and pres- sures at the level of the groundwater system and b) Local Conceptual Model (LCM), which supports parameterization of the whole groundwater system through the description of heterogeneities of the system components at a site scale and through identification of the relevant flow and solute param- eters in both the unsaturated and saturated zones. Keywords: aquifer system; area; assessment; background; boundary; concentrations; conditions; croatica; et al; european; flow; geologia; groundwater; groundwater system; levels; model; nakić; pollution; processes; quality; risk; river; romić; sava; soil; sources; status; system; zagreb; zagreb aquifer; zone
• Definition of the river Gacka springs subcatchment areas on the basis of hydrogeological parameters by Lukač Reberski, Jasmina; Marković, Tamara; Nakić, Zoran (2012) - Spring waters of Tonković, Klanac and Pećina belong to the Ca-HCO3 type of water. Spring waters are mostly saturated with calcite, which enables deposition of any existing metals in the water due to their affinity with carbonates. Keywords: analysis; aquifer; area; catchment; characteristics; discharge; gacka springs; karst; klanac; majerovo; pećina; precipitation; recession; river; river gacka; springs; springs catchment; time; tonković; vrilo; water
• Geochemical properties of topsoil around the open coal mine and Oslomej thermoelectric power plant, R. Macedonia by Stafilov, Trajče; Šajn, Robert; Sulejmani, Florije; Bačeva, Katerina (2014) - At each sampling point, soil samples were collected as top- soil (0–5 cm). For digestion of soil samples, open wet digestion with a mixture of acids was applied. Keywords: area; distribution; elements; factor; kičevo; km2; samples; soil; values
• Statistical characterization of the hydrochemical data’s of groundwater in the arid land of Wadi AdDawasir area, Saudi Arabia : A probabilistic assessment by Nazzal, Yousef Habous; Al-Arifi, Nassir; Zumlot, Taisser; Kishawy, Hossam (2014) - Skewness measures the presence of a tail deviating from a normal distribution (0) toward lower values (negative skewness) or higher values (positive skewness). As can be seen, some parameters have high values, which are reflected in the histograms by data being located on the left of the di- agram. Keywords: arabia; area; ca2; data; distribution; groundwater; mg2; parameters; saudi; study; tds; values
• The analysis of the flysch badlands inventory in central Istria, Croatia by Gulam, Vlatko; Pollak, Davor; Podolszki, Laszlo (2013) - Boljun badland catchment area on which the anal- ysis was undertaken is 1.33 km2. [The erosion of flysch badlands in the central Istria – in Croatian].– Keywords: analysis; area; badland; bedding; catchment; channel; croatica; cross; development; erosion; fig; flow; flysch; istria; processes; research
• Terrestrial Heat Flow Density in the Zagreb – Karlovac Area by Kovačić, Miron (2014) - The deposits are imperme- Figure 2: Terrestrial Heat Flow Density map of investigated area. For most of the studied area, THFD is in accordance with the mean values for continental areas. Keywords: area; flow; geothermal; heat; map; thfd; zagreb
• Modeling microfracture geometry to the asses the function of a karst system (Vízfő spring catchment area, Western Mecsek Mountains, Hungary) by Bauer, Marton; Tóth M., Tivadar (2015) - WU, q. & KULATILAKE, P.H.S.W. (2012): rEV and its properties on fracture system and mechanical properties and an orthotropic con- stitutive model for a jointed rock mass in a dam site in China.– Com- puters and Geotechnics, 43, 124–142. These mo- delling approaches combine a dissolution algorithm, a flow and/or transport model and an algorithm to reconstruct the spatial geometry of fracture networks. Keywords: area; caves; croatica; data; distribution; flow; fracture; geometry; karst; mecsek; modelling; network; porosity; spring; system; type; vízfő; water
• Multivariate statistical analysis of urban soil contamination by heavy metals at selected industrial locations in the Greater Toronto area, Canada by Nazzal, Yousef Habous; Al-Arifi, Nassir S. N.; Jafri, Muhammad Kamran; Kishawy, Hossam; Ghrefat, Habes A; El-Waheidi, Mahmoud M; Batayneh, Awni T.; Zumlot, Taisser A (2015) - GALLAGHER, F.J., PECHMANN, I., BOGDEN, J.D., GRABOSKY, J. & WEIS, P. (2008): Soil metal concentration and vegetative as- semblage structure in an urban brownfield.– Environmental Pollu- tion, 153, 351–361. 00971509620945; fax. 0097125860183) 2 Faculty of Engineering and Applied Science, University of Ontario Institute of Technology, 2000 Simcoe Street North, Oshawa, Ontario, L1H 7K4, Canada 3 Department of Earth and Environmental Sciences,Yarmouk University, Irbid 21163, Jordan doi:10.4154/gc.2015.10 ABSTRACT A good understanding of urban soils metal contamination and locating their pollution sources due to industrialization and urbanization is important for addressing environmental problems. Keywords: analysis; area; canada; concentrations; contamination; et al; locations; metals; ontario; pollution; samples; soil; table; toronto; values
• Environmental changes in the lower Mirna River valley (Istria, Croatia) during Upper Holocene by Felja, Igor; Fontana, Alessandro; Furlani, Stefano; Bajraktarević, Zlatan; Paradžik, Anja; Topalović, Ena; Rossato, Sandro; Ćosović, Vlasta; Juračić, Mladen (2015) - We interpreted this facies as outer lagoon /estu- arine conditions, in a subtidal environment influenced by freshwater inputs related to Mirna River activity. Keywords: sedimentary facies, karstic estuary, lagoon, bay head delta, foraminifers, radiocarbon age, Adriatic Sea where steep coasts are common and the coastline is often strongly indented (FURLANI et al., 2014). Keywords: adriatic; area; clay; core; croatica; deposits; et al; facies; fig; holocene; lagoon; late; level; mirna; present; river; sea; species; valley
• Evaluation of research in a bauxite-bearing area at the „Crvene stijene" locality with emphasis on exploitation of the associated deposits by Galić, Ivo; Krasić, Dragan; Dragičević, Ivan (2015) - – Proin 21 d.o.o., Široki Brijeg, 40 p. GALIĆ, I. (2002): Mining Design using specialized software, Master’s thesis, Faculty of Mining, geology and Petroleum Engineering, Zagreb, 95 p. GALIĆ, I., DRAGIČEVIĆ, I.I., ŽIVKOVIĆ, S.A., JANKOVIĆ, B., RADO- VAC, T., KOVACSICS, Á., HEDERICS, J., PODANYI, T. & HAJSEK, D. (2006): The main mining project of exploitation bauxite deposits on Bešpelj (In Croatian). In this work we analyze the „Crvene stijene“ loca- lity near Jajce in Bosnia and Herzegovina, which was studied for bauxite deposits throughout its long exploration history (Fig. 1), while other associated deposits, (that can be a sig- nificant resource), were neglected. Keywords: approach; area; bauxite; crvene; deposits; dimension; research; stijene; stone; total
• Palaeofluid evolution in a fractured basalt hosted reservoir in the Üllés-Ruzsa-Bordány area, southern sector of the Pannonian Basin by Szabó, Barbara; Schubert, Félix; M. Tóth, Tivadar; Steinbach, Gábor (2016) - THIÉRY, R., PIRONON, J., WALGENWITZ, F. & MONTEL, F. (2002): Individual characterization of petroleum fluid inclusions (composition and P­T trapping con- ditions) by microthermometry and confocal laser scanning microscopy: inferen ces from applied thermodynamics of oils.– Mar. Petrol. (1998) or APLIN et al. (1999), who used the systematic change in homogenization temperature (Th) and vapour volume fraction (φvap)values of petroleum inclusions in order to estimate the pressure of hydrocarbon migration. Keywords: analcime; anl; area; basalt; et al; fluid; fracture; hc2; heulandite; hydrocarbon; inclusions; minerals; oil; petroleum; phase; rock; szabó; temperature; type; veins; ° c
• Porphyry Cu mineralizations related with the small Tertiary volcanic intrusions in the Bučim ore deposit, Eastern Macedonia by Serafimovski, Todor; Tasev, Goran; Strmić Palinkaš, Sabina; Palinkaš, Ladislav A.; Gjorgjiev, Lazar (2016) - Keywords: Bučim, ore deposit, porphyry, Re- public of Macedonia Article history: Received September 14, 2015 Revised and accepted January 05, 2016 Avaliable online February 29, 2016 101-119 12 Figs. The formation of ore deposits was related to certain chronologi- cal stages and geo dy na mic set- tings: (1) Late Permian-Early Tri- assic intracontinental rifting along the northern bou ndary of Gondwa- na and/or its previously detached fragments; (2) Jurassic oceaniza- tion marked by the ophiolitic com- plex; (3) suprasubduction magma- tism; and (4) a postcollisional (oroge nic) continental setting and related formation of various base- and noble-metal deposits (Pb-Zn- Ag, Cu-Au, Au-As-Sb-TI, Au-Ag) (JANKOVIĆ, 1997). Keywords: area; borov; bučim; bučim deposit; bučim ore; chalcopyrite; d. l.; data; deposit; dol; et al; fluid; geol; hydrothermal; inclusions; isotope; macedonia; mineralization; minerals; ore; ore body; ore deposit; ore mineralization; phase; porphyry; quartz; range; rocks; serafimovski; sulfur; temperatures; volcanic; čifliganec
• Palaeobiogeography of the Late Carboniferous brachiopoda from Velebit Mt. (Croatia) by Japundžić, Mirko; Sremac, Jasenka (2016) - The Distribution of the Late Carboniferous cosmopolitan brachiopod genera (Neospirifer, Derbya, Chonetes, observed in Velebit Mt. (records from: PED- ERSON, 1954; SUTHERLAND, 1991; KORA, 1995; KALASHNIKOV, 1998; SOBOLEV et al., 1998; WENDT et al., 2001; SCHNEIDER, 2003; GONG et al., 2007; http://fossil- works.org/ and references therein). Distribution of the Late Carboniferous specialist brachiopod genera (Echinoconchus, Megousia, Transennatia, observed in Velebit Mt. (observations from: PEDERSON, 1954; SANDO et al., 1975; SCHNEIDER, 2003; GONG et al., 2007; HEIM et al., 2009; http://fossilworks.org/ and references therein). Keywords: area; brachiopod; carboniferous; croatia; fig; geološki; salopek; sremac; taxa; velebit
• Application of innovative technologies in landslide research in the area of the City of Zagreb (Croatia, Europe) by Mihalić Arbanas, Snježana; Krkač, Martin; Bernat, Sanja (2016) - In the framework of the described landslide research, the biggest landslide in the Podsljeme Zone, the Kostanjek landslide (landslide area of 1 km2), was also equipped with an automated near-real time moni- toring system that encompassed approximately 40 sensors to monitor landslide movement and landslide causal factors. An analysis of the spatial distribution of landslides per- formed by PODOLSZKI (2014) shows that two geomorphologi- cal historical inventories from 1967 (ŠIKIĆ, 1967) and 2007 (MIKLIN et al., 2007) contain inconsistent and unreliable land- slide data because of an underestimated number of landslides and overestimated landslide areas. Keywords: arbanas; area; city; croatia; data; engineering; et al; identification; inventory; kostanjek landslide; landslide; landslide area; mapping; mihalić; monitoring; movement; slope; surface; zagreb; zone
• Fissidentalium badense (PARTSCH in HÖRNES, 1856) from the Badenian deposits of the south and southwestern margin of the Pannonian Basin System (Central Paratethys) by Jovanović, Gordana; Bošnjak, Marija (2016) - Due to the re­ corded and afore­mentioned findings, possible migration routes of F. badense to the area of Paratethys could be the southwestern („Transtethyan corridor“) and the northern marine passages (e.g. RÖGL, 1998; STUDENCKA et al., 1998; KOVÁČ et al., 2007). At the southern margin of Central Paratethys, F. badense is recorded in the Lower Badenian deposits of Serbia (wider Bel­ grade region) Keywords: area; badenian; badense; croatian; dentalium; fissidentalium; history; hörnes; miocene; paratethys; partsch; species; specimens; zagreb
• Application of the geodiversity index for the assessment of geodiversity in urban areas: an example of the Belgrade city area, Serbia by Ilić, Marina; Stojković, Sanja; Rundić, Ljupko; Ćalić, Jelena; Sandić, Dejan (2016) - Unlike the uninhabited areas, prominent constitu- ents of geodiversity of urban areas also include anthropogenic Application of the geodiversity index for the assessment of geodiversity in urban areas: an example of the Belgrade city area, Serbia Marina M. Ilić1,*, Sanja Stojković2, Ljupko Rundić3, Jelena Ćalić4 and Dejan Sandić2 1 PhD student,University of Belgrade, Studenski trg 1, Belgrade, Serbia; (corresponding author: mrnilic@yahoo.com) 2 University of Belgrade, Faculty of Geography, Studenski trg 3/3, Belgrade, Serbia 3 University of Belgrade, Faculty of Mining and Geology, Đušina 7, Belgrade, Serbia 4 Geographical Institute „Jovan Cvijić” of the Serbian Academy of Sciences and Arts, Đure Jakšića 9, Belgrade, Serbia doi: 10.4154/gc.2016.27 Abstract (A) Shaded hypsometric map (SCILANDS, 2015) and the position of Belgrade city area; (B) A satellite map of the studied area (GOOGLE EARTH, 2009); (C) Morphological and spatial (low land and hilly) map of the studied area (MILITARY GEOGRAPHICAL INSTITUTE, 1989); (D) The administrative division of the terri- tory of the city of Belgrade. Keywords: area; assessment; belgrade; beograd; city; data; development; elements; et al; filipović; geodiversity; map; relief; serbian; soil; territory
• Factor analysis applied to distinguish influences of parent material, mining industry and agriculture on the groundwater in the Strumica valley, Macedonia by Boev, Ivan; Šorša, Ajka; Kovačević, Biljana; Mitrev, Saša; Boev, Blažo (2016) - The spatial distribution of factor scores of factor 2 is divided by separation lines running north north­east – south south­west which passed through Murtino (Fig. 4). Spatial distribution of factor scores of Factor 1. Keywords: area; data; factor; factor scores; groundwater; ilovica; macedonia; scores; strumica; valley
• Upper Cretaceous geosites on Golija Mountain - objects of geoheritage by Grujičić-Tešić, Ljiljana; Rabrenović, Dragoman; Kovačević, Jovan; Gerzina, Nataša; Đerić, Nevenka (2016) - Lying over low­grade metamorphosed schists of Carboniferous age, Upper Cretaceous rudist limestone makes a conspicuous, more than 500 m long scarp along a relatively steep slope (Fig. 2). Scarp composed of Upper Cretaceous rudist limestone, Svilanovo village. Keywords: area; cretaceous; et al; geoheritage; geosites; golija; limestone; localities; locality; mountain; rudist; serbia; values; vujičić
• Occurrence of vivianite in alluvial Quaternary sediments in the area of Sesvete (Zagreb, Croatia) by Grizelj, Anita; Bakrač, Koraljka; Horvat, Marija; Avanić, Radovan; Hećimović, Ivan (2017) - Within the investigated sediments of the boreholes, the deep blue mineral vivianite was Occurrence of vivianite in alluvial Quaternary sediments in the area of Sesvete (Zagreb, Croatia) Occurrence of vivianite in alluvial Quaternary sediments in the area of Sesvete (Zagreb, Croatia) 43 the Middle and Upper Miocene post-rift phase was marked by subsidence caused by cooling of the lithosphere (HORVÁTH & ROYDEN, 1981; ROYDEN et al., 1983; ROYDEN, 1988, PAVELIĆ, 2001). Keywords: analysis; area; basin; croatian; doi; et al; facies; fig; formation; medvednica; rocks; samples; sediments; silts; vivianite; zagreb
• The relationship of the geological framework to the Quaternary aquifer system in the Sava River valley (Croatia) by Brkić, Željka (2017) - Location of the Pan­ nonian basin showing the po­ sition of the Sava basin and Sava River valley (simplified after Horváth, 1993). Along the southern margin, the maximum depth to Article history: Manuscript received February 02, 2017 Revised manuscript accepted May 05, 2017 Available online October 31, 2017 Keywords: lithological composition, alluvial fan, Quaternary aquifer, hydrogeological characteristics, Sava River, Croatia Figure 1. Keywords: aquifer; area; basin; croatian; fig; geol; groundwater; pleistocene; quaternary; river; river valley; sava; sava river; sediments; system; valley; zagreb
• An estimation of groundwater type and origin of the complex karst catchment using hydrological and hydrogeochemical parameters: A case study of the Gacka river springs by Lukač Reberski, Jasmina; Kapelj, Sanja; Terzić, Josip (2009) - University of Zagreb, 148 p. GUAY, B.E., EASTOE, C.J., BASSET, R. & LONG, A. (2006): Identi- fying sources of groundwater in the lower Colorado River valley, USA, with δ18O, δD, and 3H: implications for river water account- ing.– Hydrogeol. In the catchment area of the Korana, they were considerably higher than in other catchment areas. Keywords: area; catchment; catchment area; croatica; data; gacka; groundwater; karst; pećina; river; springs; surface; temperature; values; water
• Evaluations of the downward velocity of soil water movement in the unsaturated zone in a groundwater recharge area using δ18 O tracer: the Kumamoto region, southern Japan by Okumura, Azusa; Hosono, Takahiro; Boateng, Dennis; Shimada, Jun (2018) - Evaluations of the downward velocity of soil water movement in the unsaturated zone in a groundwater recharge area ... 73 APPENDIX Table A1 Isotope composition of soil water in each core. The cores were cut into 0.1 m pieces and soil water was extracted from each to analyze for δD and the δ18O content. Keywords: area; core; depth; flow; groundwater; isotope; kumamoto; n.d; phase; precipitation; rate; recharge; soil; soil water; velocity; water; zone; δ18o
• The role of geology in the spatial prediction of soil properties in the watershed of Lake Balaton, Hungary by Kassai, Piroska; Sisák, István (2018) - Furthermore, with the help of prediction models infor- mation may be obtained on areas where soil data are limited or soil surveys have never been conducted. térbeli reprezentativitás-vizsgálata [Presentation of soil data from the National Pedological and Crop Production Database and investigations on spatial representativeness – in Hungarian].– Keywords: area; classification; content; data; geology; information; land; maps; models; properties; sio2; soil; soil properties; variables; watershed
• Physical, chemical and biological characterization as support for water governance in a hydrogeological system of Colombia by Ossa Valencia, Juliana; Betancur Vargas, Teresita; Duque, Jhon Camilo; Cardona Pérez, Angel Jose; Pineda Zapata, Laura; Villegas Yepes, Pedro Pablo; Paredes Zúñiga, Vanessa; Molano Cajigas, Carlos (2018) - During the calibration exer­ cise, it was possible to detect that the model is more sensitive to recharge (The recharge values calibrated in the three periods de­ fined for the year 2011 are presented in Table 2) and water level in the rivers, since these generate significant ascents or descents in the aquifer’s piezometric levels. In ad- dition, by determining the natural background level, the concentration ranges of chemical com- pounds from natural sources were obtained, in order to detect future changes in water quality. Keywords: aquifer; area; chemical; colombia; flow; groundwater; levels; model; modelling; samples; study; system; urabá; water
• Preliminary regional landslide susceptibility assessment using limited data by Peshevski, Igor; Jovanovski, Milorad; Abolmasov, Biljana; Papic, Jovan; Đurić, Uroš; Marjanović, Miloš; Haque, Ubydul; Nedelkovska, Natasha (2019) - | www.geologia-croatica.hr Journal of the Croatian Geological Survey and the Croatian Geological Society 1. INTRODUCTION Plenty of landslide susceptibility models have been developed by using GIS technology within the past three decades. Landslide susceptibility models are cat- egorized according to various criteria, and always denoted as: quantitative or qualitative, direct or indirect, heuristic, probabi- listic or deterministic, for differentiated or undifferentiated types of landslide mechanism. Keywords: area; conditioning; data; doi; et al; landslide susceptibility; landslides; low; mapping; maps; models; r*0.175; rating; region; sensitivity; study; tlsr
• Stratigraphic implications of the Mio-Pliocene geodynamics in the area of Mt. Avala: new evidence from Torlak Hill and Beli Potok (Belgrade, Serbia) by Rundić, Ljupko; Ganic, Meri; Knezevic, Slobodan; Radivojevic, Dejan; Radonjic, Milos (2019) - At the beginning of the Miocene, the studied area was rep- resented by continental-lacustrine facies of different ages (DOLIĆ, 1997, 1998; KRSTIĆ et al., 2012; RUNDIĆ et al., 2013, 2015). Seven million years later, Lake Pannon was filled with la- custrine and fluvio-deltaic sediments derived from the surround- ing orogenic belts (e.g. MAGYAR et al., 2013; RADIVOJEVIĆ & RUNDIĆ, 2016). Keywords: area; avala; badenian; basin; beli; doi; et al; fault; fig; knežević; marović; miocene; pannonian; pliocene; potok; rakovica; rundić; section; sediments; serbian; torlak
• On the origin of both a recent and submerged tombolo on Prvić Island in the Kvarner area (Adriatic Sea, Croatia) by Benac, Čedomir; Bočić, Neven; Ružić, Igor (2019) - The edges of this form are built of submerged beach sediments. This has created conditions for forming beach sediment bodies between the Njivice Rock and Prvić Island. Keywords: adriatic; area; cape; coast; doi; fig; island; level; pipa; prvić; sea; tombolo; wave
• Campanian–Early Eocene Stratigraphy of the Southern Galala Plateau, Eastern Desert, Egypt by Ismail, Ahmed Aly; Hussein Kamel, Yasmen Hussein Kamel; Boukhary, Mohamed; Ghandour, Ahmed Abdel Aziz (2008) - subramondi DE LA HARPE in the Palaeo- cene–Early Eocene sediments (Southern Galala Formation). 4 A field photograph showing the Sudr Chalk (SC) Formation and the unconformably overlying Southern Galala Formation (SG). Keywords: area; campanian; deposit; fig; figs; foraminifera; formation; galala; galala formation; maastrichtian; palaeocene; sample; section; southern; study; umm
• Geological and structural setting of the Vinodol Valley (NW Adriatic, Croatia): insights into its tectonic evolution based on structural investigations by Palenik, Damir; Matičec, Dubravko; Fuček, Ladislav; Matoš, Bojan; Herak, Marijan; Vlahović, Igor (2019) - The second reverse fault plane group (NE/RF2) observed along the NE margin of the VFZ was characterised by conjugate fault planes with a general NE–SW strike, dipping towards the NW and SE (c. 60° and 63°), indicating NW- and SE-directed G eologia C roatica Palenik et al.: Geological and structural setting of the Vinodol Valley (NW Adriatic, Croatia): insights into its tectonic evolution based on structural investigations 181 to the past and present stress fields, we used data of field meas- urements of dip direction and dip angle of fault planes and orien- tation of carbonate slickensides defined by azimuth and plunge, and, wherever possible, their sense of movement. Keywords: area; et al; fault; fault planes; field; fig; geological; group; reverse; slip; strike; study; tectonic; valley; vfz; vinodol; vinodol valley
• The prediction of structural fractures in coal seams of the Kuba coalfield, China: an application for coalbed methane (CBM) recovery development by Zhang, Zhou; Zhoua, Min; Cao, Yun-Xing; Xian, Bao-An; Gao, Di (2019) - Existing studies on fracture systems mainly observe pores and fractures by sampling hand specimens or rock and coal cores from boreholes or distinguish and predict coal fractures utilizing geophysical methods or mathe- matical simulation (YAO et al., 2009; KORONCZ et al., 2017). Characteristics of the fracture system in coal seams are among the driving factors for the explo­ ration and development of CBM (LI et al., 2013; ZHANG et al., 2017). Keywords: area; cbm; coal; coal seams; density; development; figure; fractures; kuba; relationship; rocks; strata; stress; thickness
• Integrated 3D modeling of Quaternary sediments in the Beijing Plain, based on a sequential indicator simulation by Ai, Xiao; Sun, Baitao; Chen, Xiangzhao (2019) - WEI, L.Y., PENG, G. & YAN, F.H. (1997): Climatic changes and their environmental effects during the last deglaciation in Beijing area.– ZHAO, S.J., CHENG, J., YIN, G.M. & ZAN, L.H. (2008): Palynological assemblages and palaeoclimatic significance in Beijing plain area since the Middle Pleistocene.– Journal of Palaeogeography, 110/16, 637–646. ZHAO, S.X. & LIU, Y.J. (2007): 3D Visualizing of active fault surveying data.– Seis- mology and Geology, 29/4, 787–795. ZHAO, X.T., SUN, X.P. & ZHANG, Y.L. (1984): The palaeogeographic evolution since 30000 years ago in Beijing plain. Keywords: area; beijing; data; direction; geological; model; modeling; plain; quaternary; sediments; study; variogram
• Geological conditions and gas-bearing evaluation of the Niutitang Formation shale in the Xixiang–Zhenba area, China by Xie, Qing; Xu, Feng; Wang, Ning; Yang, Zhen (2020) - LU et al. (1995) determined that the illite in clay minerals was particularly important for the ad- sorption of shale gas in shales with low organic carbon content. The pore types mainly included intragranular pores, intergranular pores, and or- ganic pores, providing good spaces for the storage of shale gas. Keywords: area; basin; characteristics; china; content; fig; formation; formation shale; gas; niutitang; pores; reservoir; shale; shale gas; study
• Application of high-resolution remote sensing technology for the iron ore deposits of the West Kunlun Mountains in China by Fan, Yuhai; Wang, Hui; Yang, Xingke; Zhang, Guofeng; Li, Zhaoyang; Tan, Furong; Zhang, Shaopeng; Wang, Wenbo (2021) - Remote sensing image features of iron ore bodies in Taxkorgan ((a) Quickbird; (b) Laobing iron mine; (c) WorldView–2 and; (d) Zoukebengou iron mine). Iron ore bodies were located mostly in the middle and lower part of the mineralization zone, with dark reddish-brown tone, narrow strip, lenticular, beaded, and intermittent exten- sion, whereas the boundary with the mineralization zone was clear. Keywords: abstract; area; band; belt; body; china; chinese; data; english; et al; image; information; iron; iron ore; kunlun; mineralization; ore; resolution; schist; sensing; wang; west
• Application of an airborne hyper-spectral survey system CASI/SASI in the gold-silver-lead-zinc ore district of Huaniushan, Gansu, China by Fan, Yuhai; Wan, Yuiqing; Wang, Hui; Yang, Xingke; Liang, Min; Pan, Chunjuan; Zhang, Shaopeng; Wang, Wenbo; Tan, Furong (2021) - (in Chinese). XIANG, A.Q., LIANG, J., CHU, N., WANG, R.J., LU, Y. & LIU, B.H. (2015): Air- borne hyper-spectral mineral mapping and prospecting prediction in the Kalat- age area, Xinjiang.– Mineral Exploration, 6/5, 586–593. ZHAO, S.-H., ZHANG, F., WANG, Q., YAO, Y.-J., WANG, Z.-T. & YOU, D.-A. (2013): Application of hyper-spectral remote sensing technology in environmen- tal protection. Keywords: abstract; alteration; area; casi; chinese; data; doi; et al; gold; hyperspectral; mineral; ore; remote; rock; sasi; sensing; silver; study; wang
• Sedimentary and structural setting of the Aptian reservoir deposits in the Kasserine area, west-central Tunisia by Lazzez, Khaled; Lazzez, Marzouk; Ben Fadhel, Moez; Ben Rabah, Ramla; Zouaghi, Taher (2020) - Previous stratigraphic and sedimentological studies have contributed to interpretations of Cretaceous palaeogeography in west-central Tunisia (Fig. 3), which is considered to represent a large transitional zone between the platform to the south, and a deep trough to the north (e.g. BIS- MUTH et al., 1981, MARIE et al., 1984, ZGHAL, 1994; BEN- ZARTI, 2002; LAZZEZ et al., 2008; BEN FADHEL et al., 2011; ZOUAGHI et al., 2011). The early Aptian is outlined by the emergence of Kairouan Island that took place in central Tunisia. Keywords: aptian; area; ben; central; des; et al; formation; reservoir; tunisia; west; zouaghi
• Landslide types in the Slani Potok gully, Croatia by Jagodnik, Petra; Jagodnik, Vedran; Arbanas, Željko; Mihalić Arbanas, Snježana (2020) - Despite the importance of landslides for the local communities and policies, it has been estimated that landslide maps cover less than 1% of the slopes in the landmasses, and that systematic in- formation on landslide types, their spatial distribution and sta- tistics is lacking (GUZZETTI et al., 2012; MIHALIĆ ARBANAS & ARBANAS, 2014). Landslide inventory map of the Slani Potok gully presented on the semi-transparent (80%) Keywords: area; debris; doi; et al; fig; flow; gully; hillshade; landslide; lidar; map; phenomena; potok gully; slani; slani potok; slope; study; types; valley
• Geochemical characteristics of the barite occurrences in the Paleozoic complex of the Southeastern Bosnia and their relationship to the barite deposits of the Mid-Bosnian Schist Mountains by Jurković, Ivan; Garašić, Vesnica; Hrvatović, Hazim (2010) - This conclusion is supported by the elevated Sr content in barites of both areas (0.48 to 2.83% in SEB, 1.44% in MBSM) and the δ13C and δ18O val- ues in calcite and siderite of barite ore deposits which are shifted toward lower values relative to typical values oc- curring in the Devonian host rock. This can be explained by the lower temperature and lower salinity of mineralisation fl uids in barite ore deposits of SEB. Keywords: area; barite; barite deposits; bosnia; croatica; deposits; devonian; et al; isotope; jurković; mbsm; ore; ore deposits; palaeozoic; permian; seb; sulphides; sulphur; tetrahedrite; type; values; variscan; δ34s
• Application and improvement of soil spatial distribution mapping using advanced modelling techniques by Alijagić, Jasminka; Šajn, Robert (2020) - | www.geologia-croatica.hr Journal of the Croatian Geological Survey and the Croatian Geological Society Application and improvement of soil spatial distribution mapping using advanced modeling techniques Jasminka Alijagić* and Robert Šajn Geological Survey of Slovenia, Dimičeva ulica 14, SI–1000 Ljubljana, Slovenia; (Jasminka.Alijagic@geo-zs.si; Robert.Sajn@geo-zs.si) *corresponding author doi: 10.4154/gc.2020.01 Abstract The main purpose of this contribution is to develop realistic prediction digital soil maps in order to increase their visuality, and to evaluate and compare the performance of different modeling techniques: a) Kriging, b) Artificial Neural Network – Multilayer Perceptron (ANN-MLP) and c) Multiple Polynomial Regressions (MPR). G eologia C roatica Alijagić and Šajn: Application and improvement of soil spatial distribution mapping using advanced modeling techniques 71 into the small cities of Vareš and Breza. Keywords: area; curvature; data; digital; distribution; doi; elements; environmental; km2; kriging; mapping; maps; methods; modeling; models; soil; study; target; techniques; values

• First record of trace fossils from the Oxfordian Argiles rouges de Kheneg Formation (Tiaret, northwestern Algeria) by Belaid, Mourad ; Cherif, Amine; Vinn, Olev; Naimi, Mohammed Nadir (2020) - 2. GEOGRAPHICAL AND GEOLOGICAL FRAME- WORK Geographically, the study site belongs to the northern domain of Algeria called ”Alpine Algeria”, which consists of three domains First record of trace fossils from the Oxfordian Argiles rouges de Kheneg Formation (Tiaret, northwestern Algeria) First record of trace fossils from the Oxfordian Argiles rouges de Kheneg Formation (Tiaret, northwestern Algeria) 87 Unit C (Uppermost part of the formation - upper Ammonitico rosso) Keywords: algeria; argiles; deposits; doi; facies; fig; formation; fossils; isp; kheneg; oxfordian; trace; unit
• Correlation of upper Miocene–Pliocene Lake Pannon deposits across the Drava Basin, Croatia and Hungary by Sebe, Krisztina; Kovačić, Marijan; Magyar, Imre; Krizmanić, Krešimir; Špelić, Marko; Bigunac, Dijana; Sütő-Szentai, Mária; Kovács, Ádám; Szuromi-Korecz, Andrea; Bakrač, Koraljka; Hajek-Tadesse, Valentina; Troskot-Čorbić, Tamara; Sztanó, Orsolya (2020) - In Croatia three main lithostratigraphic schemes are in use today for upper Miocene deposits of the northern and eastern part of the country. SZTANÓ,­O.,­MAGYAR,­I.,­SZÓNOKY,­M.,­LANTOS,­M.,­MÜLLER,­P.,­LENKEY,­ L.,­KATONA,­L.­&­CSILLAG,­G.­ (2013a):­A­Tihanyi­ Formáció­ a­Balaton­ környékén:­típusszelvény,­képződési­körülmények,­rétegtani­jellemzés­[Tihany For­ mation in the surroundings of Lake Balaton: type locality, depositional setting and stratigraphy­–­in­Hungarian].–­Földtani­Közlöny,­143,­73–98. SZTANÓ,­O.,­SZAFIÁN,­P.,­MAGYAR,­I.,­HORÁNYI,­A.,­BADA,­G.,­HUGHES,­D.W.,­ HOYER,­D.L.­&­WALLIS,­R.J.­(2013b):­Aggradation­and­progradation­controlled­ clinothems­and­deep-water­sand­delivery­model­in­the­Neogene­Lake­Pannon,­Makó­ Trough,­Pannonian­Basin,­SE­Hungary.–­Global­and­Planetary­Change,­103,­ ­149–167.­doi:­10.1016/j.gloplacha.2012.05.026 SZTANÓ,­O.,­SEBE,­K.,­MAGYAR,­I.­&­CSILLAG,­G.­(2015):­Turbidites­as­indicators­ of paleotopography, Late Miocene Lake Pannon, Western Mecsek (Hungary).– Keywords: basin; correlation; croatia; deposits; drava; drava basin; eologia; etrusca; figure; formation; hungary; lake; member; miocene; mts; pannonian; pliocene; roatica; sand; sebe; sediments; spiniferites; the­
• Tidal deposits in the Early Miocene Central Paratethys: the Vučji Jarek and Čemernica members of the Macelj formation (NW Croatia) by Avanić, Radovan; Pavelic, Davor; Pécskay, Zoltan; Miknić, Mirjana; Tibljas, Darko; Wacha, Lara (2021) - The early Miocene deposition of the HZB strongly differs from the rest of north Croatia, i.e. from the rift-type North Croatian Basin (NCB), where sedimentation commenced in the Ottnan- gian and was characterized by fresh-water environments that passed into marine deposition in the early or middle Badenian (PAVELIĆ, 2001; ĆORIĆ et al., 2009; MALVIĆ, 2012; PAVELIĆ & KOVAČIĆ, 2018; AVANIĆ et al., 2018a, b; BRLEK et al., 2018, 2020). Intense volcanism produced the crystalline tuff and a high accumulation of pumice, while quieter volcanism re- sulted in vitric tuff and low accumulation of pumice (ŠIMUNIĆ, AL. et al., 1988; McPHIE et al., 1993). Keywords: avanić; basin; croatia; cross; deposition; deposits; doi; eggenburgian; et al; facies; fig; formation; geol; glauconitic; jarek; macelj; marine; material; miocene; paratethys; samples; sandstones; tidal; vučji; zagreb; čemernica; šimunić
• Geological, geochemical and fluid inclusion investigations on the Duna Pb-Ba-(Ag) deposit, Central Alborz, North Central Iran by Sadeghi, Alireza; Nezafati, Nima; Hakimi-Asiabar, Saeid; Ganji, Alireza (2022) - SAMANI RAD, S. (1999): Geology, mineralogy and genesis of Duna Pb deposit from Central Alborz.– M. Sc. Thesis, Islamic Azad University, North Tehran Branch, Iran. SAMSON, L. M. & RUSSELL, M.J. (1987): Genesis of the silvermines zinc-lead-barite deposit, Irland; fluid inclusion and stable isotope evidence.– Fluid inclusion samples were collected from open pit through the ore-bearing veins and tunnels from discordant/second stage/ younger/Irish-type (codes Dsa4 and Dsa8) and concordant/1st stage/older/MVT of mineralization. Keywords: alborz; barite; deposits; duna; et al; fig; fluid; galena; host; inclusions; iran; irish; mineralization; mvt; ore; ppm; rock; samples; stage; temperature; type
• Sedimentary record of Pleistocene aeolian - alluvial deposits on Vrgada Island (eastern Adriatic coast, Croatia) by Banak, Adriano; Pikelj, Kristina ; Lužar Oberiter, Borna; Kordić, Branko (2021) - Correlation of the possible tephra horizon from Vrgada island with tephra layers on other Adriatic islands suggests an Upper Pleistocene age for the sediment of facies A. Vrgada Island sediments composed of three different facies represent a transitional zone between the north Adriatic islands, where aeolian sediments dominate and the SEA archipelago where mixture of alluvial and aeolian sediments are observed. Sand grains were coated with a 25 nm thin gold layer and ana- lysed using a scanning electron microscope JEOL, model JSM- 6510LV. Keywords: adriatic; aeolian; alluvial; carbonate; deposits; doi; eastern; et al; facies; fig; grains; gravel; island; pleistocene; samples; sand; sediment; vrgada
• Geological potential of antimony, bauxite, fluorite, and magnesite of the Central Dinarides (Bosnia and Herzegovina): exploration and exploitation perspective by Borojević Šoštarić, Sibila; Markelj, Anže; Jašarević, Eldar; Haindl, Angelika (2022) - Sava-Vardar Zone hosting antimony deposits. As described, antimony deposits also host Zn, Ag or, in the case of Rupice, BaSO4. Keywords: + b; + c; antimony; b b; b c; barite; bauxite; bosnia; c c; data; deposits; dinarides; european; exploration; fluorite; geological; herzegovina; magnesite; materials; mining; ore; potential; region; reserves; type; zone
• The primary and secondary mineral resources of Montenegro and their mapping into the European data model by Radusinović, Slobodan; Šajn, Robert; Jovanović, Božica; Rokavec, Duška ; Hribernik, Katarina; Abramović, Vasilije; Draksler, Matej; Danilović, Ivan; Jovanović, Mia (2022) - Presentation of data on the EGDI web portal In addition to the map service displaying mineral deposits and mines on the EGDI portal, the portal also provides occurrence­ specific documents related to mineral materials, enabling users to make their own analyses from a huge amount of data (Fig.2). The basic characteristics of the most important types and depos­ its of primary mineral raw materials in Montenegro are presented here; non­metallic and energy raw materials are also included. Keywords: bauxite; coal; data; deposits; european; inspire; lead; materials; mineral; mineral resources; mining; montenegro; near; ore; pljevlja; production; radusinović; resources; rocks; tailings; waste; zinc
• The future of mining in the Adria region: current status, SWOT and Gap analysis of the mineral sector by Borojević Šoštarić, Sibila; Giannakopoulou, Stavroula; Adam, Katerina; Mileusnić, Marta (2022) - In the Early Neolithic period, the Adria region was a centre of mining and metallurgical activ- ities due to its richness in copper ore minerals such as malachite and azurite (RADIVOJEVIĆ et al. 2010). Raw material potential The Adria region mainly comprises the Dinarides, the northwest- ernmost Hellenides, and the Vardar zone, which host Palaeozoic to Neogene External and Internal units (the High Karst and Pre- Karst units, Variscan basement units with the surrounding Bos- nian flysch, the Western Vardar ophiolite unit, and the Sava su- ture zone) and ore deposits associated with various stages of the Alpine Wilson cycle (PALINKAŠ et al., 2008; PAMIĆ et al., 1998). Keywords: adria; analysis; base metals; bauxite; bosnia; class; copper; countries; deposits; et al; exploration; herzegovina; inspire; iron; lead; materials; metals; metals al; metals cu; mineral; mining; ore; potential; region; resources; sector; zinc
• Palaeoenvironmental reconstruction of Holocene calcareous tufas distributed over a manganese deposit in Mexico by Puy-Alquiza, Maria Jesus; Miranda-Avilés, Raúl; Puy, Miren Yosune Miranda ; Kshirsagar, Pooja Vinod ; Zanor, Gabriela A. ; Del Rincon- Castro, Ma. Cristina (2024) - Calcareous tufa deposits correspond to carbonate for- mations of inactive tufas disconnected from the current hydrological network. The 14C analysis indicates that the plant found in the charcoal sample within the calcareous tufa deposit is of Holocene age. & VILES (1994) and ARENAS-ABAD (2017), several factors are required for calcareous tufa deposits to form: warm climate; physicochemical processes favourable for carbonate precipitation; organic structural elements; tectonics; and characteristics of the substrate (lithological composition). Keywords: analysis; calcareous; calcareous tufa; calcite; carbonate; deposits; doi; environment; et al; facies; formation; holocene; manganese; mexico; molango; plants; samples; tufa; tufa deposits; water
• Croatian Critical Mineral Commodity Letters: Magnesium by Borojević Šoštarić, Sibila; Tomašić, Nenad; Bohanek, Vječislav ; Gizdavec, Nikola; Miko, Slobodan (2025) - Although production of magne­ sium from dolomite is associated with high environmental impacts and is mainly conducted in China, it is important to note that dolomite is suitable for magnesium production using the Pidgeon process. Considering the high atmospheric emissions and the high­ energy consumption in magnesium production, it is unlikely that the production of magnesium from dolomite will take place on EU territory. Keywords: applications; carbonate; content; costs; croatian; deposits; dolomite; dolostone; extraction; industry; jurassic; limestone; magnesite; magnesium; magnesium sources; materials; mineral; mining; potential; process; production; rocks; sources; wt%
• Tracing the evolution of the world's first mined bauxite from palaeotopography to pyritization: insights from Minjera deposits, Istria, Croatia by Perković, Ivor; Martinuš, Maja; Cvetko Tešović, Blanka; Vlahović, Igor; Matešić, Darko; J. Newton, Robert; He, Tianchen ; Šoufek, Marin; Razum, Ivan; Durn, Goran (2024) - More than 10,000 bauxite occurrences and small bauxite deposits are known in Istria (Milan Mihovilović, pers. Intense karstification occurred especially along fractured zones, resulting in numerous smaller and larger sinkholes and decametre-sized karstic canyons that served as sediment traps for the accumulation of the source material for bauxite formation. Keywords: bauxite; bauxite deposits; carbonate; colloform; content; d-15; deposits; doi; earth; elements; et al; evolution; fig; figs; formation; geology; iron; istria; karst; matrix; minjera; pyrite; red; sample; values
• Geochemical Map of Croatia – Key findings and legacy of geochemical mapping in the Pannonian Basin by Pjanić, Ajka; Halamić, Josip; Galović, Lidija; Peh, Zoran (2025) - Soil groups BOGUNOVIĆ et al. (1998) harmonised the Croatian pedological nomenclature with the FAO nomenclature and published the FAO UNESCO pedological map of the Republic of Croatia (Fig. 3c, d) represent a collection of soil groups with their associated geochemical imprints originating from various soil­forming processes characteristic of the Croatian PAN region. Keywords: analysis; areas; basin; cambisols; clastic; clc; cover; croatia; data; deposits; df2; discriminant; et al; fig; function; geology; gora; group; land; leptosols; map; model; pannonian; peh; rocks; sampling; sediments; soil; table
• Abiogenic, microbial and hybrid authigenic crusts: components of Precambrian stromatolites by Riding, Robert (2008) - This suggests that Sparry Crust stromatolites are essentially abiogenic aqueous precipitates, in the sense that their formation does not require biotic pro cesses and that they do not typically contain organically generated fabrics. Hybrid Crusts consist of millimetric alternations of these fabrics, in layers that are more regular than those usually present in Fine-grained stromatolites, and less regular than those of Sparry Crust stromatolites (Fig. 12). Keywords: abiogenic; calcite; canada; carbonate; cement; components; crust; crust stromatolites; dark; day; deposits; et al; examples; fabrics; fi g.; formation; geologia; grains; grotzinger; group; hybrid; james; knoll; laminae; late; layers; marine; mats; microbial; oor; precambrian; precipitation; proterozoic; riding; seafl; sediment; sparry; sparry crust; stromatolites; sumner
• Middle Miocene (Upper Badenian/Sarmatian) Palaeoecology and Evolution of the Environments in the Area of Medvednica Mt. (North Croatia) by Vrsaljko, Davor; Pavelić, Davor; Miknić, Mirjana; Brkić, Mato; Kovačić, Marijan; Hećimović, Ivan; Hajek-Tadesse, Valentina; Avanić, Radovan; Kurtanjek, Nenad (2010) - Upper Badenian deposits are approximately 30 to 70 m thick on the slopes of Medvednica Mt., and the maximum thickness of the Sarmatian deposits is 50 m (after BASCH, 1983). 2. GEOLOGICAL SETTING Miocene deposits of the investigated area belong palaeo- geographically to the south-western margins of Central Paratethys (Figs. 1 & 2), and geotectonically to the Pan- nonian Basin System (PAVELIĆ, 2001). Keywords: association; badenian; central; deposition; deposits; facies; fig; foraminifera; medvednica; miocene; paratethys; sarmatian
• The Benkovac Stone Member of the Promina Formation: A Late Eocene Succession of Storm-Dominated Shelf Deposits by Mrinjek, Ervin; Pencinger, Vili; Sremac, Jasenka; Lukšić, Boris (2010) - The sporadic occurrence of gutter casts at the bases of Facies S1 beds may theo- retically be due to either oscillatory waves or combined- flow currents (MYROW & SOUTHARD, 1996). Facies S3: sandstone beds with convolute stratification Keywords: beds; benkovac; cross; deposits; division; facies; fig; figs; formation; log; member; mudstone; promina; sandstone; storm; transition; zone
• The Origin and Importance of the Dolomite-Limestone Breccia Between the Lower and Upper Cretaceous Deposits of the Adriatic Carbonate Platform: An Example from Ćićarija Mt. (Istria, Croatia) by Vlahović, Igor; Tišljar, Josip; Fuček, Ladislav; Oštrić, Nenad; Prtoljan, Božo; Velić, Ivo; Matičec, Dubravko (2010) - However, within the breccia zone there are also spatially restricted occurrences representing relics of breccia deposits of specific origin, also caused more or less directly by recurring intense tectonic activity during post-Cretaceous tectonic phases (Tertiary tecton- ic phase and Neotectonic phase): a) tectonic breccia; b) stylolitization breccia; c) collapse breccia. On the basis of the occurrence of dolomite-lime- stone breccias of ∆iÊarija Mt., their composition and structural-textural characteristics, as well as the com- plex tectonic and diagenetic processes relevant to their formation the following main conclusions may be drawn: 1) these rocks are not sedimentary, intrabasinal brec- cias formed by synsedimentary tectonic phases between the Lower and Middle Cretaceous; 2) the investigated sequence of breccia deposits repre- sent a continuous succession located within the structure of ∆iÊarija Mt. between the Upper Albian and Middle to Upper Cenomanian deposits, i.e. they are not equivalent to a tectogenous rock fall breccia of the Jelar type (Cenozoic breccia covering large areas of Velebit Mt. and some of the northern Adri- atic islands - BAHUN, 1974); 3) the studied sequence represents rocks of specific properties and origin, formed by complex tectonic and diagenetic processes affecting a specific litho- logical succession different from neighbouring units - besides other specific breccia types recognised within the studied sequence, most of the rocks could be referred to as post-sedimentary tectogenic-diage- netic breccia formed in situ. Keywords: breccia; carbonate; deposits; diagenetic; dolomite; fig; fragments; limestone; origin; rocks
• Water Reservoir Within the Karst Field Overburden: Gusić Polje, Croatia by Pavičić, Ante; Benamatić, Davor; Pešt, Damir; Marasović, Marijan (2010) - First of these appearances was the ponor in the bottom of the basin, with diameter of 2 m and depth of over 3 m. The fol- lowing appearances had diameters up to 5 m and depth up to 6 m. Several causes for water loss were supposed - poor construction or non existence of clay carpet in the zone of the canal, as well as the existence of ponors underneath the Quaternary deposits. By subsequent construction of the clay carpet, the losses were reduced, and additional losses are attributed to lack of clay carpet below the supply canal and Fig. 1 Location map and hydrogeological map of the GusiÊ Polje reservoir. Keywords: basin; carpet; clay; deposits; gusiê; polje; ponors; potential; water
• The Palaeogeography of Lake Pannon During Deposition of the Congeria rhomboidea Beds by Gulyas Jr., Sandor (2001) - The gradual evolution of Congeria rhomboidea M. HÖRNES f r o m Congeria zsigmondyi and a relation with C o n g e r i a p a r t s c h In order to draw the boundaries of a given facies marked by the geographical distributions of specimens of Congeria rhomboidea M. HÖRNES or the P r o s o - d a c n o m y a genus, the maximal area of their distribution had to be considered by taking into account their mar- ginal occurrences. Keywords: basin; budapest; congeria; deposits; fig; lake; pannonian; r o; rhomboidea; species
• Calcareous algae, foraminifera and sequence stratigraphy of the Fahliyan Formation at Kuh-e-Surmeh (Zagros Basin, SW of Iran) by Hosseini, Seyed Abolfazl; Conrad, Marc A. (2008) - I ?Deabarina hahounerensis FOURCADE et al., Valanginian, sampe JHT 1343. Only two surface samples were prepared from the limestone horizons of this formation which are dominated by: Palorbitolina lenticularis BLUMENBACH, Salpingopore- lla dinarica RADOIČIĆ, Debarina hahounerensis FOURCADE et al., Choffatella decipiens SCHLUMBERGER, Trocholina sagittaria ARNAUD-VANNEAU et al, T. oduk paniensis DES- SAUVAGIE, Aulotortus sp., Novalesia distorta ARNAUD- VANNEAU, Dukhania sp., Falsogaudryinella tealbyensis BARTENSTEIN, Dukhnia conica HENSON and oncoids of Lithocodium aggregatum ELLIOTT with Bacinella irregula- ris RADOIČIĆ, associated with echinoid remains, mollusc fragments and corals. Keywords: algae; berriasian; deposits; fig; foraminifera; formation; geologia; radoičić; ramp; salpingoporella; sample jht; sequence; valanginian
• Lower Miocene Alluvial Deposits of the Požeška Mt. (Pannonian Basin, Northern Croatia): Cycles, Megacycles and Tectonic Implications by Pavelić, Davor; Kovačić, Marijan (2010) - Deposits in the measured sections were grouped into nine facies units: 1) massive matrix-supported con- glomerates (Gmu - plastic debris flow), 2) massive 69PaveliÊ & KovaËiÊ: Lower Miocene Alluvial Deposits of the Poæeπka Mt. ... For explanation of the facies codes see Table 1. 71PaveliÊ & KovaËiÊ: Lower Miocene Alluvial Deposits of the Poæeπka Mt. ... ates deposited by gravitational mechanisms (Gmu and Gmi) occur in various parts of the cycles, from the basal and middle to the upper part, irrespective of the trend. Keywords: alluvial; basin; deposits; facies; fan; fig; miocene; parica; poæeπka
• Lithocodium and Bacinella signature of a late Hauterivian, local microbial event: the Urgonian limestone in South-East France by Conrad, Marc A.; Clavel, Bernard (2008) - L: large fragment of Lithocodium crust. Epifl uorescence tests In the layer with Lithocodium and Bacinella, the binding-trap- ping mechanism is primarily performed by Lithocodium crusts, Bacinella, and other micro-encrusters denoting an open ma- rine habitat, and by fi ne-grained, organo-mineralic deposits conceivably generated by microbes. Keywords: bacinella; clavel; deposits; dolomite; hauterivian; jura; layer; lithocodium; parasequence; platform; tract; urgonien
• Nearshore Deposits in the Middle Eocene Clastic Succession in Northern Dalmatia (Dinarides, Croatia) by Babić, Ljubomir; Zupanič, Jožica (2010) - what lower in the shore face, as they are inte rcalated between storm sandstone beds inferred to reflect such an ellvironment (see above). (eM) Main conglomerates Description The above title embraces several facies, and inclu­ des combinations of superimposed conglomerate beds, which differ from one another mainly in clast size and shape. Keywords: angle; arc; babic; basal; beach; beds; clastic; clasts; coarse; conglomerate; con­; cross; deposits; eocene; facies; fig; geol; gravel; hcs; ing; ion; laminated; lamination; low; marine; middle; nearshore; nummulites; parea; processes; radovin; sandstone; sandy; sediments; shoreface; storm; unit; zone; zupanic
• Upper Aptian calcareous algae from Padurea Craiului (Northern Apuseni mountains, Romania) by Bucur, Ioan I.; Granier, Bruno; Sasaran, Emanoil (2008) - M. Kogălniceanu nr.1, 400084 Cluj-Napoca, Romania; ( ibucur@bioge.ubbcluj.ro; esasaran@bioge.ubbcluj.ro) 2 Département des Sciences de la Terre, UFR des Sciences et Techniques, Université de Bretagne Occidentale (UBO), 6, avenue Le Gorgeu, F-29238 Brest Cedex 3, France; (bgranier@univ-brest.fr) Upper Aptian calcareous algae from Pădurea Craiului (Northern Apuseni Mountains, Romania) Upper Aptian calcareous algae from Pădurea Craiului 299 3. Keywords: algae; aptian; bucur; craiului; cretaceous; croatica; deposits; fig; formation; geologia; limestone; pădurea; species
• The Middle and Upper Permian Deposits in Gorski Kotar: Facts and Misconceptions by Aljinović, Dunja; Sremac, Jasenka (2010) - The problem whether Upper Permian rocks do or do not occur in Gorski Kotar, conscquently raises the ques­ tion of a continuous or di scontinuous transition at the Permo-Lower Triassic boundary. REVIEW OF PREVIOUS STUDIES Previous studies of Palaeozoic rocks in the Gorski Kotar region have been aimed mainly towards the dif­ ferentiation of the principal rock types, their mapping, and the description of mapped units which are some­ times termed as facies (Fig. Keywords: alps; beds; boundary; clastic; complex; conglomerates; deposits; devide; facies; fig; gorski; gorski kotar; groden; ihe; kochansky; kotar; limestone; lower; middle; palaeozoic; permian; ramoys; red; region; rocks; salopek; sandstone; susnjara; thc; tion; transition; triassic; type; upper; zagreb
• The Development of the Eocene Platform Carbonates from Wells in the Middle Adriatic Off-Shore Area, Croatia by Tari Kovačić, Vlasta (2010) - They developed on the very edge of the platform toward the slope and basin, and they are laterally and vertically (Waltcr' s Law) the first neighbouring member of facies E and G of the transgressive sequence. Facies G was studied in mechan ica l cores in Kate-! Keywords: arc; carbonate; deposits; environment; eocene; facies; fig; gamma; grainstone; jadran-9; kate; kornati; limestone; log; mud; mudstone; oil; packstone; platform; porosity; sedimentary; sediments; sequence; susak; wells
• Cobalt, nickel, wolfram, cadmium, selenium, silver and gold-bearing mercurian tetrahedrite from the Saski Rad barite-siderite deposit in the Mid-Bosnian Schist Mts. by Jurković, Ivan B.; Garašić, Vesnica; Jurković, Ivan M. (2011) - Saski R. barite SEB–B barite Kreševo fl uorite ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ΣREE 183.1 159.5 216.5 158.8 59.5 33.0 15.6 9.15 8.4 5.14 0.416 La 38.0 29.4 33.1 36.8 9.8 5.9 2.9 8.19 1.8 1.30 0.026 Ce 76.8 64.8 74.6 60.1 23.7 4.9 5.5 0.64 0.3 0.24 Keywords: barite; bosnia; deposits; jurković; jurković et; maškara; mbsm; n.a; ore; ppm; ppm ppm; rad; saski; saski rad; siderite; tetrahedrite; type; wt.%
• Travertines and calcareous tufa deposits: an insight into diagenesis by Golubić, Stjepko; Violante, Crescenzo; Plenković-Moraj, Anđelka; Grgasović, Tonći (2008) - These developments derive from the growth preferences and adaptive capacity of aquatic mosses (Pl. 2, Fig. 1), which are in that sense the real architects of cold water travertine deposits (ARENAS et al., 2000). 9 Doric temple in Paestum, southern Italy, built of ambient water travertine that preserves aquatic mosses. Keywords: calcifi; carbonate; cyanobacteria; deposition; deposits; diagenesis; fig; geologia; golubic; growth; oocardium; plitvice; scale; system; travertine; tufa; water
• gc-44 by None (None) - The Paratethys Sea fl ooded the new basins successively dur- ing the Karpatian (late Burdigalian, Early Miocene) and the Early Badenian (middle Langhian, Middle Miocene). Keywords: Pannonian Basin System, North Croatian Basins, Central Paratethys, Dinaride Lake System, Middle Miocene, biostratigraphy 1 Geological Survey of Austria, Neulingg. Keywords: badenian; basin; c r; central; croatian; deposits; geol; karpatian; marine; middle; miocene; north; paratethys; pavelić; r f; r r; rögl; section; system; zagreb
• Correlation of Quaternary Sediments and Tectonic Activity of the Eastern Part of the Drava River Depression by Prelogović, Eduard; Velić, Josipa (2010) - Sveobuhvatnije su kvartarne naslage podvrgnute istraživanju u okviru prikupljanja podataka za gradnju hidroelektrana na Dravi. Prvo, u većem dijelu depresije naslage su deblje od 200 m, mjestimice iznad 300 m, a između Kapelne Keywords: beograd; boundary; deposits; depresije; depression; drava; dravske; faults; fig; geol; karta; l l; marker; naslaga; prelogović; ras; sediments; zagreb; zavod
• Sedimentary bodies, forms and occurrences in the Tudorevo and Mirovo glacial deposits of northern Velebit (Croatia) by Velić, Josipa; Velić, Ivo; Kljajo, Dubravka (2011) - Till Tills have been widespread in central and southern parts of Tudorevo, in Dundović Mirovo, Bilensko Mirovo and at Bilo hill. At that time it covered Tudorevo, Dundović Mirovo and Bilensko Mirovo, reaching Baričević Dolac where it deposited a terminal moraine, the current Bilo hill. Keywords: bilensko; clasts; deposits; dundović; fig; glacier; jurassic; limestones; mirovo; moraine; terminal; till; tudorevo
• Geochemical characteristics of mercurian tetrahedrite, barite and fluorite from the Duboki Vagan, Glumac and Dubrave-Dugi Dol barite deposits, south of Kreševo, Mid-Bosnian Schist Mts. by Jurković, Ivan B.; Garašić, Vesnica; Jurković, Ivan (2011) - This is all in the accordance with the possible existence of two different paragenetic types of barite deposits in the MBSM and SEB (Southeastern Bosnia), which signifi - cantly differ in the δ18OSMOW ranges of their barites and δ34SCDT values of their sulphides. In the Mid-Bosnian Schist Mountains (MBSM) and South- eastern Bosnia (SEB) two completely different paragenetic types of barite deposits occur. Keywords: barite; barite deposits; deposits; duboki; et al; jurković; jurković et; ore; ppm; ree; sample; tetrahedrite; uorite; vagan; values
• Hydrodynamic characteristics of Mt. Biokovo foothill springs in Croatia by Kuhta, Mladen; Brkić, Željka; Stroj, Andrej (2011) - Keywords: karst hydrogeology, spring hydrograph, time series analysis, Biokovo Hydrodynamic characteristics of Mt. Biokovo foothill springs in Croatia � Mladen Kuhta, Andrej Stroj and Željka Brkić Department of Hydrogeology and Engineering Geology, Croatian Geological Survey, Sachsova 2, 10 000 Zagreb, Croatia; (mkuhta@hgi-cgs.hr, astroj@hgi-cgs.hr, zbrkic@hgi-cgs.hr) doi: 104154/gc.2012.03 Geologia Croatica 65/1 Analysis of the spring hydrograph using auto- correlation and cross-correlation functions Time series analyses in karst hydrogeology are used to de- termine karst system characteristics, to investigate the rela- tionships between spring discharge and rainfall and between discharge, to continuously measure physico-chemical pa- rameters and to assess the interdependence of discharge in several springs (MANGIN, 1984; PADILLA & PULIDO- BOSCH, 1995; LAROCQUE et al. 1998; PANAGOPULOUS & LAMBRAKIS, 2006; KOVAČIČ, 2010). Keywords: biokovo; characteristics; deposits; discharge; fast; fl ow; izbitac; karst; makarski; recession; spring; system; time; vrutak; water
• Laterally variable development of a basin-wide transgressive unit of the North Dalmatian foreland basin (Eocene, Dinarides, Croatia) by Babić, Ljubomir; Zupanič, Jožica (2012) - The remaining part of the succession is organised cycli- cally, with ideal cycles consisting of limestone units and coarsening-upward (CU) units (Figs. 7, 8). Examples of partial cycles include the alternation of limestone units and lower parts of CU units (e.g. 46–56.6m in Fig. 7), and probable repetitions of lower-to-upper clino- form facies. Keywords: babić; basin; beachface; beds; calcarenites; conglomerates; croatica; deposits; fig; figs; foraminifera; foreland; limestones; marine; middle; mudstones; section; stratigraphic; succession; surface; type; unit; upper; zupanič
• Taxonomy and stratigraphy of an algal assemblage in Palaeogene deposits of the northern foothills of Mt. Biokovo (Southern Croatia) by Sokač, Branko; Velić, Ivo; Grgasović, Tonći; Ćosović, Vlasta; Vlahović, Igor (2012) - 1 Longitudinal–oblique section of three connected segments, slide SB–17E1/1. 6 Oblique section of a segment with branches visible in two levels, slide RAK–40B/3. 7 Longitudinal–oblique section of two connected segments; visible position of the branches in two or three close whorls, slide RAK–40A/5. 8 Longitudinal section of two connected segments with branches in the levels of upper constrictions, slide RAK–40A/10. Keywords: algal; assemblage; barattolo; branches; clypeina; croatica; deposits; falsolikanella; fig; figs; geologia; oblique; romano; section; slide; species; thallus; transverse; whorls; x22
• Influence of terrestrial sedimentation in Pennsylvanian rocks of Croatia by Sremac, Jasenka (2012) - Carbon- iferous areas in Croatia were presented as sheets and in ex- planatory booklets Crikvenica L33-102 (GRIMANI et al., 1970, 1973), Daruvar L33-95 (JAMIČIĆ, 1989; JAMIČIĆ et al., 1989), Delnice L33-90 (SAVIĆ & DOZET, 1985 a,b), Gospić L33-127 (SOKAČ et al., 1974, 1976a), Ivanić-Grad L33-81 (BASCH 1981, 1983), Obrovac L33-140 (IVA- NOVIĆ et al. 1973, 1976), Orahovica L33-96, JAMIČIĆ & BRKIĆ, 1988; JAMIČIĆ et al., 1987), Udbina L33-128 (ŠUŠNJAR et al., 1973; SOKAČ et al., 1976b) and Zagreb L34-98 (ŠIKIĆ et al., 1978, 1979). Velebit Mt. and the Lika Region The most complete succession of clastic and carbonate de- posits from the Pennsylvanian (Moscovian) to the end of the Permian and the beginning of the Triassic (RAMOVŠ et al., 1990; SREMAC, 2005), can be derived from an elongate ca. Keywords: croatia; deposits; et al; flora; geološki; l33; map; palaeozoic; pennsylvanian; region; rocks; velebit; zagreb; zavod
• Environmental geochemistry of the polymetallic ore deposits: Case studies from the Rude and the Sv. Jakob historical mining sites, NW Croatia by Strmić Palinkaš, Sabina; Palinkaš, Ladislav A.; Kuzmanović, Maja; Martinić, Maša; Kampić, Štefica; Dogančić, Dragana; Obhođaš, Jasmina (2013) - Furthermore, the study revealed that the populated areas (stream waters with decreased redox potential, increased organic matter content, high NO3 –, NH4 + and PO4 3– con- centrations; stream sediments enriched in exchangeable Pb and Zn) and the Sava river alluvium (overfl owing streams enriched in Hg) represent a greater environmental threat than the investigated polymetallic ore deposits. Keywords: polymetallic ore deposits, exchangeable metals, stream water, stream sediments, Samoborska Gora Mts., Medvednica Mts., NW Croatia. Keywords: concentrations; content; creek; d.l; deposits; et al; gradna; metals; ore; potok; rudarska; rude; sediments; stream; triassic; veliki; water
• Macropalaeontology and stratigraphy of lacustrine Miocene deposits at Crnika beach on the Island of Pag (Croatia) by Bulić, Jeronim; Jurišić-Polšak, Zlata (2009) - Miocene deposits are rich in fossil remains of bivalves, gastropods, some higher and lower plants, as well as other organisms that populated the one-time lake and its shore. They are overlain by an alternation of thin strata of yellow Fi gu re 3: Outcrops of Miocene deposits along the beach Crnika. Keywords: beach; coal; congeria; crnika; croatica; deposits; figs; genus; geologia; island; kochansky; lake; marls; material; miocene; outcrop; pag; profi; remains; sample; shell; species; specimens
• Dinaride evaporite mélange: Diagenesis of the Kosovo polje evaporites by Kulušić, Anita; Borojević Šostarić, Sibila (2014) - ORTÍ, F., ROSELL, L. & ANADÓN, P. (2010): Diagenetic gypsum re- lated to sulfur deposits in evaporites (Libros Gypsum, Miocene, NE Spain).– Sedim. Rauhwacke are composed of partly dedolomitized dolostone and leached gypsum fragments, cemented with late stage calcite. Keywords: adriatic; anhydrite; breccia; carbonate; cover; croatica; deposits; dolomite; evaporite; formation; fragments; gypsum; halite; kosovo; mélange; opq; planar; polje; type
• Permian–polysulphide-siderite–barite–haematite deposit Rude in Samoborska Gora Mts., Zagorje–Transdanubian zone of the Inner Dinarides by Palinkaš, Ladislav A.; Borojevic Sostaric, Sibila; Strmić Palinkaš, Sabina; Prochaska, Walter; Spangenberg, Jorge; Cuna, Stella; Šinkovec, Boris (2010) - Petrol., 59, 41–93. KÖPPEL, V. (1983): Summary of lead isotope data from ore deposits of the Eastern and Southern Alps: Some metallogenetic and geotec- tonic Implications.– The stratabound siderite–pyrite–barite–quartz ore consists of an iron ore layer extending more than 1.5 km in the NE–SW direction. Keywords: barite; croatica; deposits; fig; galena; gora; gypsum; haematite; late; mineralisation; mts; ore; permian; polysulphide; pyrite; quartz; rude; siderite; stratabound; stratiform; uid; veins
• Planktonic foraminiferal biostratigraphy and paleoecology of Upper Cretaceous deposits from the Palmyride Region, Syria by Pecimotika, Gabrijela; Cvetko Tešović, Blanka; Premec Fućek, Vlasta (2014) - PEARSON, P.N., DITCHFIELD, P.W., SIGNANO, J., HARCOURT- BROWN, K.G., NICHOLAS, C.J., OLSSON, R.K., SHACKLE- TON, N.J. & HALL, M.A. (2001): Warm tropical sea surface tem- peratures in the late Cretaceous Eocene epochs: Nature, 413, 481–487. PETRIZZO, M.R. (2002): Palaeoceanographic and palaeoclimatic infer- ences from Late Cretaceous planktonic foraminiferal assemblages from the Exmouth Plateau (ODP Sites 762 and 763, eastern Indian Ocean).– Many studies have focused on biostratigraphic evolution of Cretaceous planktonic foraminifera (e.g., ROBASZYN- SKI et al., 1984; 2000; CARON, 1985; SLITER, 1989; RO- BASZYNSKI & CARON, 1995; PETRIZZO, 2003; PRE­ MO LI SILVA & VERGA, 2004; SARI, 2006, 2009; BABA ZADEH et al., 2007; HUBER et al., 2008; PETRIZZO et al., 2011; GARDIN et al., 2012). Keywords: assemblage; biozone; campanian; cretaceous; croatica; deposits; et al; figs; foraminifera; formation; heterohelix; interval; maastrichtian; mahr-1; muricohedbergella; palmyra-1; palmyride; planktonic; pseudoguembelina; silva; species; syria
• Fluid inclusion study of the Boccassuolo VMS-related stockwork deposit (Northern-Apennine ophiolites, Italy) by Kiss, Gabriella B.; Garuti, Giorgio; Zaccarini, Federica (2015) - wt%, NEHLIG, 1991 and JUTEAU et al., 2000). This stockwork mineralisation consists of pyrite, chalcopyrite, and sphalerite, with (in the upper levels), galena, occurring together with quartz, calcite and chlorite (see e.g. GARUTI et al., 2008, 2011 and the re‑ ferences therein). Keywords: boccassuolo; chlorite; deposits; et al; fig; fluid; formation; garuti; hydrothermal; inclusions; ophiolites; quartz; site; stockwork; sulphide; temperature; type; veins
• Obituary Professor emeritus Ivan Jurković (1917-2014) by Garašić, Vesnica; Durn, Goran (2015) - JURKOVIć B. I., GARAŠIć, V. & JURKOVIć M. I. (2011): Geochem- ical characteristics of mercurian tetrahedrite, barite and fluorite from the barite deposits Duboki Vagan and Dubrave-Dugi Dol, south of the town of Kreševo, Mid-Bosnian Schist Mountains.– He was the leading mineral resource geologist in the countries of the former Yugoslavia where he pioneered both the use of ore microscopy in the study of ore deposits and the under- standing of their genesis in the relation to the global tectonic paradigm. Keywords: barite; bosnia; croatian; croatica; deposits; dinarides; geol; geološko; jurković; meeting; mid; mountains; naftni; ore; ore deposits; palinkaš; professor jurković; tunisie; university; vjesnik; yugoslavia; zagreb; zbornik
• Stratigraphic and paleogeographic significance of lacustrine mollusks from the Pliocene Viviparus beds in central Croatia by Mandic, Oleg; Kurečić, Tomislav; Neubauer, Thomas A.; Harzhauser, Mathias (2015) - “Neritina semi­ plicata” sensu HOERNES (1877) from the Late Messinian (�AGATAY et al., 2006) or Early Pliocene (MELINTE-DO-�AGATAY et al., 2006) or Early Pliocene (MELINTE-DO-et al., 2006) or Early Pliocene (MELINTE-DO- BRINESCU et al., 2009) The threefold strati- graphic classification into the lower, middle and upper Vivi­ parus beds is well established throughout the region, sup- ported by the biostratigraphic zonation of Viviparus species (NEUMAYR & PAUL, 1875; PENECKE,1884; JENKO, 1944; OŽEGOVIĆ, 1944; TAKŠIĆ, 1954; MARINESCU & PAPAIANOPOL, 1995; LUBENESCU & LUBENESCU, 2008). Keywords: 1874a; basin; beds; brusina; central; cernikian; croatia; dacian; deposits; der; des; et al; figs; figure; fuchsi; geol; geologia; height; kravarsko; lake; material; melanopsis; middle; miocene; neumayr; non; pannonian; papaianopol; paul; penecke; pleistocene; pliocene; sample; shell; slavonia; species; specimens; stratigraphic; theodoxus; type; und; valvata; viviparus; vukotinovici; wenz; whorls; zone
• Genetic concepts on the formation of the Austrian magnesite and siderite mineralizations in the Eastern Alps of Austria by Prochaska, Walter (2016) - Genetic concepts on the formation of the Austrian magnesite and siderite mineralizations in the Eastern Alps of Austria Walter Prochaska University of Leoben, Department of Geological Sciences, A-8700 Leoben, Austria 32 Vol. 69/1 during recent decades some considerable progress was made in the understanding of these mineralizations using modern scien- tific methods. NIEDER- MAYR (1989) argued for synsedimentary or early diagenetic genesis for magnesite mineralization in the Permian series of the Eastern Alps and extended this model to the alpine sparry mag- nesites. Keywords: age; alps; deposits; eastern; fluids; formation; host; hydrothermal; magnesite; mineralizations; ore; prochaska; siderite; zone
• Plate tectonic aspects of the Triassic carbonate-hosted stratiform-stratabound base-metal deposits in the Western Balkan, NW Bulgaria by Marinova, Irina; Damyanov, Zhelyazko (2015) - In: Problems of ore deposits formation, Vth Sympo- sium, Varna, 2, 13−25. ATANASOV, V. (1972): Mineralogy of the copper-lead-zinc stratiform Sedmo- chislenitsi deposit, Bulgaria.– PhD thesis, Institute of Geology and Geo- physics, Siberian branch of the Russian Academy of Sciences, Novosibirsk, 398 p. (in Russian). ATANASOV, V. (1973): On the structure and natural boundaries of the Sedmo- chislenitsi copper-lead-zinc deposit, Western Stara Planina Mt.– Annual Higher Inst. Geochemistry of hydrothermal ore deposits, Wiley, New york, 509−567. PALINKAŠ, L., DAMyANOV, Z., BOROjeVIĆ, S., STRIMIC, S. & MARI- NOVA, I. (2014): Divergent rifting separation of Adriatic-Dinaric and Moe- sian carbonate platforms witnessed by Triassic MVT and SeDeX deposits, Metallogenic approach.− Proc. Keywords: balkan; barite; base; bulgarian; carbonate; damyanov; deposits; district; kremikovtsi; metal; ore; rocks; stratiform; triassic; vratsa
• The Ljubija geothermal field: A herald of the Pangea break-up (NW Bosnia and Herzegovina) by Palinkaš, Ladislav; Borojević Šoštarić, Sibila; Strmić Palinkaš, Sabina; Prochaska, Walter; Pécskay, Zoltan; Neubauer, Franz; Spangenberg, Jorge E (2016) - This impressive collection of fluid inclusion types, (more than 9 in one single crystal) requires multistage episodes of boiling producing a mixture of liquid water and bubbles, suspension of crystalls, halite, sylvite, and unknown solids, trapped into one single crystal. Selection of fluid inclusion types in one single crystal of fluorite, Žune- Dolinac locality (PALINKAŠ, 1988). Keywords: adamuša; age; barite; dark; deposits; dinarides; et al; field; fig; fluid; fluorite; geothermal; high; hydrothermal; iii; inclusions; ljubija; ljubija ore; locality; melting; metasomatic; mineral; nacl; ore; palaeozoic; palinkaš; permian; quartz; range; salinity; samples; siderite; temperature; type; vein; water; zebra; zebra siderite
• The Mineral Resources of the Bor Metallogenic Zone: A Review by Jelenković, Rade; Milovanović, Dragan; Koželj, Dejan; Banješević, Miodrag (2016) - This supports the earlier mentioned discovery of copper-gold mine ralization in the Brestovac ore field and in the deeper part of the Borska reka porphyry copper deposit in the Bor system. doi: 10.1007/BF00204503 JANKOVIĆ, S. (1980): Metallogenic features of copper deposits in the volcano- intrusive complexes of the Bor district, Yugoslavia.– Keywords: andesite; bor; complex; copper; deposits; gold; metallogenic; mineral; mineral resources; mineralization; ore; porphyry; resources; rocks; serbia; timok; type; zone
• Divergent drift of Adriatic-Dinaridic and Moesian carbonate platforms during the rifting phase witnessed by triassic MVT Pb-Zn and SEDEX deposits; a metallogenic approach by Palinkaš, Ladislav; Damyanov, Zhelyazko K.; Borojević Šoštarić, Sibila; Strmić Palinkaš, Sabina; Marinova, Irina (2016) - The scenario is outlined by the symmetrical distribution of ore deposits characteristic for the rifting metallogenesis, MVT Pb-Zn ores in carbonates (Bleiberg-Mežica type) and SEDEX iron-manganese-polymetallic ore sediments (Red Sea type). [Formation of mineral ore deposits in SR Slovenia– in Slovenian].– Geologija, 23/1, 1–157, Ljubljana. Keywords: carbonate; deposits; ore; palinkaš; rifting; sedex; triassic
• A cave response to environmental changes in the Late Pleistocene: a study of Budimirica Cave sediments, Macedonia by Temovski, Marjan; Pruner, Petr; Hercman, Helena; Bosák, Pavel (2016) - The response of the cave to Late Pleistocene environmental changes is interpreted based on a detailed study of cave sediments, with previous data being supplemented, reinterpreted and compared to the Ohrid Lake palaeoclimate record. This can lead to the absence of cave sediments from certain time­periods in whole regions, e.g. Middle Pleistocene sediments are missing in caves of the Bohemian Karst (central Czech Republic; HORÁČEK & LOŽEK, 1988). Keywords: budimirica; budimirica cave; cave; cave sediments; changes; deposits; flowstone; incision; kamenica; mis; pleistocene; profile; river; sediments; temovski; valley
• The Alpine Wilson cycle and NW Tethyan Metallogeny by Palinkaš, Ladislav A.; Bermanec, Vladimir; Galović, Lidija (2016) - Their diversification brings plethora of phenomena in tectonism, magmatism, sedimentary facies and ore deposit formation. In the century of revolutionary affirmation of global tecto­ nics as deus ex machina of orogenesis, Ivan Jurković without hesitation accepted its principles and bravely incorporated Wilson cycle into the studies of ore deposits in Dinarides. Keywords: deposits; formation; metallogenic; ore; rifting; zone
• In Memoriam Professor Emeritus Ivan Jurković by Palinkaš, Ladislav; Bermanec, Vladimir (2016) - New hypothesis concerning the Hercynian metallogeny in the Dinarides In the period from 2007 to 2011, Jurković was first to use the previously unapplied modern geochemical and other physi- co-chemical analyses to the investigation of rhyolites and minerals from the all paragenetic types of ore deposits in the 173 Palinkaš & Bermanec: In the same year (1966) Jurković, with the agreement of UN, studied (for three weeks) huge lead­zinc bearing barite deposits in the region of Ouida, Eastern Mo- rocco, on account of comparison with Tunisian deposits. Keywords: barite; council; croatian; deposits; faculty; geology; jurković; member; ore; professor; science; university; zagreb
• Early Eocene evolution of carbonate depositional environments recorded in the Čikola Canyon (North Dalmatian Foreland Basin, Croatia) by Španiček, Jelena; Ćosović, Vlasta; Mrinjek, Ervin; Vlahović, Igor (2017) - Schematic correlation of Cretaceous to Palaeogene carbonate and clastic successions in the area of the Dinarides (for location see Fig. 1), from NW to SE: (1) Kras region (modified after DROBNE & PAVŠIĆ, 1991; ŽIVKOVIĆ & BABIĆ, 2003; ZAMAGNI et al., 2008); (2) Istria (modified after BENIĆ, 1991; DROBNE & PAVLOVEC, 1991; ĆOSOVIĆ et al., 2004); (3) Korlat–Benkovac section (modified after IVANOVIĆ et al., 1976; DROBNE et al., 1991); (4) Skradin–Dubravice section (modified after MAMUŽIĆ, 1975; DROBNE et al., 1991; MARJANAC & ĆOSOVIĆ, 2000); (5) Čikola section (this paper); (6) Hvar, Podstina section (modified after PUŠKARIĆ, 1997; MAR­ JANAC et al., 1998; PAVŠIČ & PREMEC FUČEK, 2000: SCHWEITZER et al., 2007; KORBAR et al., 2015), and (7) Pelješac, Orebić section (modified after MARJANAC et al., 1998). The microfacies types and foramini- feral assemblages enabled interpretation of the palaeoenviron­ mental conditions of the studied deposits similar to existing car­ bonate-ramp models (BUXTON & PEDLEY, 1989; BURCHETTE & WRIGHT, 1992; GEEL, 2000; POMAR, 2001; ROMERO et al., 2002; BASSI, 2005; BOSENCE, 2005; ZAMAGNI et al., 2008; TOMASSETTI et al., 2016). Keywords: basin; beds; carbonate; deposits; doi; drobne; environments; eocene; et al; evolution; fig; foraminifera; mft; microfacies; middle; miliolids; palaeogene; ramp; section; shallow; unit; čikola
• A mineralogical-petrographical study of evaporites from Mali Kukor, Vranjkovići and Slane Stine quarry (Upper Permian evaporites from Dalmatia, Croatia) by Dedić, Željko; Ilijanić, Nikolina; Miko, Slobodan (2018) - Alabastrine and porphy- roblastic types most probably correspond to the upper phreatic groundwater zones, while the appearance of gypsum on, or near to, the surface, as well as the presence of anhydrite in deeper parts, reflects the fact that secondary gypsum minerals are the result of anhydrite hydration. These se- diments can be subdivided into three members, a lower evaporite unit (an anhydrite member), a middle evaporite unit (a gypsum member), and an upper unit (a clastic member), and are main- ly comprised of secondary gypsum that formed via the hydration of precursor anhydrite rocks. Keywords: anhydrite; carbonate; crystals; deposits; dolomite; evaporite; gypsum; kukor; mali; middle; permian; samples; study; vranjkovići
• Biostratigraphy of the Konkian (Middle Miocene of the Eastern Paratethys) deposits of Southern Ukraine based on foraminifera by Vernyhorova, Yuliia (2018) - Predominance of Konkian euryhaline species and presence of a small number of the early Sarmatian species (e.g. E. dissita dissita, Obsoletiforma lithopodolica ruthenica; their shells have small sizes) A variety of molluscs and foraminiferal Konkian assemblages that have different paleoecological characteristics. The distribution of Konkian foraminiferal assemblages in more deep-water deposits of the Kerch Peninsula is significantly different from deposits of the coeval shallow-water sediments of the Northern Black Sea Region and the Crimean Peninsula. Keywords: assemblages; beds; black; deposits; eastern; ervilia; euryhaline; foraminifera; kerch; konkian; miocene; molluscs; paratethys; peninsula; region; russian; sea; shells; species; ukraine; vernyhorova; wells
• Megabeds in Istrian Flysch as markers of synsedimentary tectonics within the Dinaric foredeep (Croatia) by Petrinjak, Krešimir; Budić, Marko; Bergant, Stanislav; Korbar, Tvrtko (2021) - Rare bauxite and karstified Cretaceous limestone clasts were only reco- gnised in the Kaldir megabed. Limestone clasts were distinguished according to DUNHAM’s (1962) classifica- tion modified by EMBRY & KLOVAN (1971). Keywords: basin; breccia; carbonate; clasts; cretaceous; deposits; division; doi; eocene; et al; facies; fig; flysch; hum; istrian; limestones; marl; matrix; megabeds; middle; section

• Sorption of cadmium, zinc and copper in dominant soils of the Zagreb aquifer system, Croatia by Kovač, Zoran; Ružičić, Stanko; Rubinić, Vedran; Nakić, Zoran; Sertić, Marcel (2022) - The result of the sorption experiments in texturally different soils confirmed that soil sorption decreased in the order Cu > Also, soil pH can have the greatest ef- fect of any single parameter on the mobility or retention of me- tals, with a greater retention and lower solubility of metal cations that occur at high soil pH (MARTINEZ & MOTTO, 2000). Keywords: cec; content; doi; horizons; profile; ptms; soils; sorption; values; zagreb
• Taxonomic revision of the Lake Pannon cockle subgenus Lymnocardium (Budmania) BRUSINA, 1897 by Magyar, Imre; Katona, Lajos (2023) - L. ferrugineum was a shallow-water dweller in Lake Pannon, whereas L. cristagalli populated offshore, sublittoral environ- ments. Remarks: The syntypes of L. ferrugineum hold some uncer- tainty, because their original labels were lost. Keywords: brusina; budmania; cristagalli; ferrugineum; fig; figs; lake; lymnocardium; magyar; pannon; roth; semseyi; species; specimens; zagreb
• In Memoriam Josip Tišljar (1941-2009) by Vlahović, Igor; Velić, Ivo; Sokač, Branko (2010) - TADEJ, N., SLOVENEC, D. TIŠLJAR, J. & INKRET, I. (1997): Glau- conitic materials from Lower Miocene Macelj-sandstones of the Hrvatsko Zagorje, north-western Croatia.– BALEN, I., TIŠLJAR, J. & MAJER, V. (1975): Petrografske karakter- istike lapora okolice Podsuseda na jugozapadnim obroncima Med- vednice. Keywords: abstracts; adriatic; carbonate; cretaceous; croatia; dinarides; eds; geologia; geology; geološki; institute; international; istria; matičec; meeting; platform; tišljar; velić; vlahović; zagreb
• History of investigations of fossil algae in Croatia by Grgasović, Tonći (2008) - i Da- turellina nov. gen., preliminarna beleška (Large Tintinnina Camp- belliella nov. gen. and Daturellina nov. gen., a preliminary note). i Da- turellina nov. gen., preliminarna beleška (Large Tintinnina Camp- belliella nov. gen. and Daturellina nov. gen., a preliminary note). Keywords: algae; barremian; cretaceous; croatia; dasycladaceae; dasycladales; deloffre; der; des; devidé; environs; fossil; genus; geol; geologia; grgasović; gušić; herak; island; kochansky; milanović; n.sp; new; nikler; permian; pia; pls; radoičić; salpingoporella; sokač; velebit; velić; vjesnik; zagreb
• Prof.dr.sc. Slobodan Šestanović (1945–2005) by Velić, Ivo (2010) - Privreda Dalmacije, 13/3, 37–40, Split. ŠESTANOVIĆ, S. (1976): Energetski resursi Dalmacije s osvrtom na potrebu štednje BULIČIĆ, A., VUKANAC, D., BRNIČEVIĆ, B. & ŠESTA- NOVIĆ, S. (1977): Ekonomski položaj i realizacija pro- grama razvoja aluminijske industrije Dalmacije.– Privreda Dalmacije, 14/10, 4–21, Split. ŠESTANOVIĆ, S. (1977): Problematika hidroenergetskog sistema “Orlovac” s aspekta gubitaka vode iz akumulacije Buško Blato.– Privreda Dalmacije, 14/11–12, 5–9, Split. ŠESTANOVIĆ, S. (1978): Osvrt na problematiku istraživanja, eksploatacije i prerade nemetalnih sirovina Dalmacije.– Privreda Dalmacije, 15/8, 17–21, Split. ŠESTANOVIĆ, S. (1979): Mogućnost kvantitativnog defini- ranja vodopropusnosti akumulacije Buško Blato.– Zbornik radova u povodu 40-te god. Keywords: barčot; dalmacije; jug; rgn; simp; split; zagreb; zbornik; čagalj; šestanović
• Equatorial Shelf of the Palaeozoic Supercontinent – Cradle of the Adriatic Carbonate Platform by Sremac, Jasenka (2010) - On Velebit Mt. carbonate sedimentation took place for approximately 20 million years, producing a sequence of shallow-marine carbonate sediments more than 900 m thick (KOCHANSKY-DEVIDÉ, 1965; SOKAČ et al., 1976). TIŠLJAR, J., VLAHOVIĆ, I., SREMAC, J., VELIĆ, I., VESELI, V. & STANKOVIĆ, D. (1991): Excursion A – Velebit Mt. Permian–Jurassic.– Keywords: carbonate; carboniferous; croatia; devidé; geol; kochansky; middle; palaeozoic; permian; ramovš; sediments; sremac; triassic; velebit; zagreb
• Verification of Engineering-Geological/Geotechnical Correlation Column and Reference Level of Correlation (RNK) Method by Observations in the Slip-Plane Zone by Jurak, Vladimir; Ortolan, Želimir A.; Slovenec, Dragutin; Mihalinec, Zlatko A. (2010) - Here, attention is drawn to the group of clay samples characterized by very high plasticity (CV) which is often typical for materials of pronounced colloidal activity and high expansivity. Results obtained through determination of the plasticity index of clay samples during all three campaigns are presented in Fig. Keywords: clay; column; correlation; engineering; fig; landslide; level; method; plane; plasticity; rnk; samples; slip; zagreb; zone
• Dean Bošković B. Sc. (1929–2003) by Matičec, Dubravko; Velić, Ivo (2010) - As a student he worked as an undergraduate assistant in the Department of the Mine- ralogy and Geology Institute and was fully committed to all activities conducted by the Institute – actively participating in field and laboratory work, in writing professional and scientific papers on geology, petrology, and mineral deposits. For years he was one of the leading people in the Institute of Geology Zagreb, a man whose work has, over time, left a significant impact on the status of our profession in Croatian society. Keywords: institute; zagreb
• Dr.sc. Jakob Pamić (1928–2004) by Gušić, Ivan (2010) - J. Earth Sci., 91, 538–554, Berlin. J. Earth Sci., 91, 787–797, Berlin. Keywords: abstracts; acta; alpine; basin; beograd; croatia; dinarida; dinarides; geol; geology; glas; jakob pamić; ophiolite; pamić; pamić pamić; pannonian; sarajevo; stijene; tomljenović; yugoslavia; zagreb; zone
• Heavy Metal (As, Cd, Cu, Hg, Pb and Zn) Distribution in Topsoil Developed on Alluvial Sediments of the Drava and Sava Rivers in NW Croatia by Halamić, Josip; Galović, Lidija; Šparica-Miko, Martina (2010) - Cumul.% 1 3.48 58.07 58.07 2 0.96 16.04 74.11 3 0.82 13.63 87.75 4 0.54 9.03 96.78 Table 9 Eigenvalues of factors for Drava River valley topsoils. Cumul.% 1 3.96 66.01 66.01 2 0.79 13.14 79.14 3 0.64 10.69 89.83 Table 5 Eigenvalues of factors for Sava River valley topsoils. Keywords: drava; metals; river; river valley; sava; sediments; topsoil; valley; values; zagreb
• The South-Western Boundary of Central Paratethys by Pavelić, Davor (2010) - KOCHANSKY-DEVIDÉ, 1976; KOCHANSKY-DEVIDÉ & SLI©KOVI∆, 1978; PAMI∆ et al., 1978; POL©AK et al., 1978; SOKA», 1980; JURI©I∆-POL©AK, 1984; RAI∆ et al., 1984; ÆAGAR-SAKA» & SAKA», 1984; JURI©I∆-POL- ©AK & SLI©KOVI∆, 1988; ©U©NJARA & SAKA», 1988; JURI©I∆-POL©AK et al., 1993; OLUJI∆, 1999). i s sp. and C a n d o n a sp.. The youngest Pliocene to Pleistocene newly determined molluscan species are Odontohydrobia croatica and Limnidia likana ( J U R I- ©I∆-POL©AK et al., 1997). Keywords: basin; geol; miocene; neogene; pannonian; paratethys; region; rögl; water; zagreb
• Dr.sc. Pero Mioč (1931- 2001) by Velić, Ivo (2010) - sudjelovao je u tim istraæivanjima prak- Geologia Croatica 55/1 103 -106 ZAGREB 2002 IN MEMORIAM Dr. sc. Sudjelovao je u istraæivanjma æeljeznih ruda u Nimbi, u afriËkoj Guineji. Keywords: geoloπka; karta; list; ljubljana; mio; osnovna; sfrj; zagreb; zavod; ænidar»i
• Interdependence of Petrophysical Properties and Depth: Some Implications of Multivariate Solution on Distinction Between the Lower Pontian Hydrocarbon-bearing Sandstone Units in the Western Part of the Sava Depression by Saftić, Bruno; Peh, Zoran; Velić, Josipa; Jüttner, Ivanka (2010) - Discriminant axes on the scatterplot of variables (Figs. 7a-b) are drawn as norma- lised vectors, while on the scatterplot of canonical means (centroid values for FIELD groups) these indi- cate an altogether different scale (Figs. 7c-d). From Fig. 11a, which illustrates depth relations (as for Fig. 10a), it can be observed that contour lines coincide with the structure contours of the southern part of Æutica field as previously illustrated by the structure contour map (Fig. 4). Keywords: data; depth; df2; df3; discriminant; distribution; field; fig; group; gss; oil; okoli; permeability; porosity; properties; reservoir; sandstone; units; values; wells; zagreb; æutica
• Ante Renić (1948-2000) by Pavičić, Ante (2010) - Sudjelovao je u izradi hidrogeoloπkih podloga mnogih objekata koji su u raznim stupnjevima projektiranja - HE KrËiÊ, HE Tisne Stine, HE Zrmanja, HE æegar, HE »ikola, HE Kosinj, HE Ombla U podruËju naπeg krπa mr. ReniÊ je bio ukljuËen u hidrogeoloπke radove na veÊini hidroenergetskih obje- kata koji se danas koriste ili je radio istraæne radove za projektnu dokumentaciju za buduÊe objekte. Keywords: ante; pavi»i∆; podruëju; radova; reni∆; voda; zagreb
• Les Algues Dasycladales du Permien et du Trias. Nouvelle tentative d’inventaire bibliographique, géographique et stratigraphique by Granier, Bruno; Grgasović, Tonći (2010) - Karrer, Pl. XVI.b, fig. Karrer, Pl. XVI.b, fig. Keywords: adige; algae; algues; alto; anisien; anisien fig; anisien supérieur; annulata; anthracoporella; apuseni; autriche; bangkok; bihor; buri; bystrický; c l; c o; c r; calcareous; carbonifère; carnien; clavaphysoporella; collection; croatica; croatie; dans; dasycladales; de diplopora; de johnson; del; der; des; devidé; diplopora; dragastan; d’amérique; d’après; e l; e o; e phra; e t; endo; epimastopora; et al; et du; et pl; extrait; extrait de; fig; figurée; flügel; friuli; fédération; g e; gen; geologia; gifu; giulia; grgasoviê; griphoporella; gun; gyroporella; gümbel; güvenç; h e; h o; h.-t; herak; herculea; honshū; iii; illyrien; inférieur; institute; italie; japon; johnson; kantia; ken; kochansky; kras; kärnten; l l; l o; ladinien; les; limestone; lombardia; m e; m o; macroporella; mince; mizzia; monténégro; moyen; mts; mura; murghabien; museum; n c; n e; n krung; n o; n s; n sara; n t; new; nom; non; norien; nud; o v; oligoporella; ou pl; p l; p r; pars; partie; pauciforata; pelsonien; permien; permien et; permien fig; permien inférieur; permien moyen; permien supérieur; physoporella; pia; pilosa; planina; postérieur de; r e; r n; r o; rhétien; roumanie; roux; russie; s e; s o; s t; saitama; sakmarien; sciences; serbie; silésien; slovaquie; slovénie; sp.endo; spectabilis; supérieur; supérieur fig; t l; t o; t r; teutloporella; thaïlande; thep; tokyo; trentino; trias; triassic; u l; u n; u r; u s; und; unis; university; vachard; val; var; velebit; venezia; vii; viii; vol; von; wettersteinkalk; wien; xiii; yougoslavie; zagreb; zone; états
• Lithologic Composition and Stratigraphy of Quaternary Sediments in the Area of the Jakuševec Waste Depository (Zagreb, Northern Croatia) by Velić, Josipa; Saftić, Bruno; Malvić, Tomislav (2010) - It was dis- covered that the silty-clayey units (units 1, 3 and 5) are covered by sandy-gravely (units 2 and 4) and gravely ones (unit 6), respectively. The gravels of units 2, 4 and 5 are clearly differing from the ones in unit 6. Keywords: composition; fig; fraction; jm-13; jm-7; mineral; pleistocene; quartz; sand; sediments; unit; veli∆; zagreb
• Seabed and Surface Sediment Map of the Kvarner Region, Adriatic Sea, Croatia (Lithological Map, 1:500,000) by Juračić, Mladen; Benac, Čedomir; Crmarić, Ranko (2010) - Red soil (terra rossa ) ubiquitous on the land in Kvarner region is polygenetic, and its distribution is a consequence of erosion and accumulation (BENAC & DURN, 1997). By lowering of the sea to the -50 m level, the cir- culation of water through Vela Vrata (the strait between Kvarner Bay and Rijeka Bay) was probably interrupted. Keywords: adriatic; bay; geol; kvarner; level; map; region; rijeka; sea; sediments; zagreb
• Upper Cretaceous - Palaeogene Tholeiitic Basalts of the Southern Margin of the Pannonian Basin: Pozeska gora Mt. (Croatia) by Belak, Mirko; Halamić, Josip; Marchig, Vesna; Tibljaš, Darko (2010) - Basic plagioclase is completely altered into acid plagioclase in approxi­ male ly 80% or the analysed rocks, while in 20 % of basalts basic plagioclase is preserved, but rarely unalte­ red, because of prehnitization and sericit ization. Basic rocks represent part of the magmatic complex of the NE part of the Pozeska gora Mt. , which is also composed of alkal i-feldspath ic granites and rhyolites (Fig. 2). Keywords: age; arc; basalts; basin; content; cretaceous; diagram; elements; fig; geol; gora; mantle; optical; palaeogene; pamic; plagioclase; pozeska; rocks; samples; table; volcanic; zagreb
• Recommendations for Landslide Hazard and Risk Mapping in Croatia by Mihalić, Snježana (2010) - In this paper, an inventory was made of the currently available methods for landslide hazard and fisk zonation, in order 10 produce recommendations for the lise of specific methods in relation to lhe sca le of analysis . The end result of haz­ ard and risk analysis should be presented in informative documents, usually in the form of various maps which display the spatial distribution of hazard and risk clas­ ses, These documents are used by decision-makers who have to define a general risk prevention policy, Many methods and techniques have been proposed for landslide hazard and risk mapping over the last 30 years (BRABB. Keywords: analysis; arc; areas; assessment; croatia; data; development; hazard; int; inventory; ion; landslide; landslide hazard; map; mapping; maps; methods; movement; planning; proc; risk; scale; slope; symp; zagreb
• Mr sc. Leon Nikler (1932 - 1997) by Bošković, Dean; Sokač, Branko (2010) - izabran jc za dircklo ra spomcnu(og zavoda, pa lu duzilosl obavlj a svc Leon NrKLER 211 POPIS OBJA VLJENIH RADOVA BIBLIOGRAPHY 1. IY ANOYIC, A., SOKAC, B. & NIKLER, L. (1962): Dber das Alter der Kalkbroksien des sud­ ostlichen Teiles des Yelebit. Keywords: acad; cons; geol; geoloska; leon; nikler; rad; sci; sfrj; sokac; zagreb
• Morphological Variability as a Basis for Palaeontological Classification by Radovčić, Jakov (2010) - 1I0t consider our material separately, rather we sheill affempt to estahlish its relation to the whole ... , writes Professor Herak, ... in this manner we shall cstablish thc systenwtic significancc of our cave hear, meaning that we shall he able to establish whe­ ther it can be considered a typical representativc (~f the species Ursl/s spelaclfs , or whcther this \ovas somc kind of new variety or race. Before we state the current judgment about this innovative work in Croatian palae­ ontology by Professor Herak, it is necessary for LIS to remember several almost general facts from the history of the palaeontological sciences. Keywords: bear; cave; herak; kramberger; krapina; variability; work; world; zagreb
• Professor Herak's Contribution to Regional Geology and Geotectonics by Benić, Josip; Blašković, Ivan; Tomić, Vladimir (2010) - Geologia Croatica 50/2 REFERENCES HERAK , M. ( 1959): Prilog geolog iji i hidrogeo logiji otoka Hvara (Zur Geologie und Hyd rogeologie der 1nsel Hvar).- GeoL vjesn ik, 12 (1958), 135- 148. HERAK , M. ( 1960): Geologija Gracackog polja u Liei (Geologie des Karst Polje von Gracac in def Lika, Kroatien).- GeoL vjesnik, 13 ( 1959), 3 1-56. HERAK, M., BOlANIC, L., SIKIC, D. & MAGDA­ LENIC, A. (196 1): Novi clement i tektonike u pod­ rucju gornjeg toka rijeke Kupe (Neuc Elcmente der Tektonik tektoniei ploca posvuda u sv i­ jetu preuzima poJozaj klasicnih koncepeija fiksizma, te jc zato na tim osnovama pokusao naei nova geotekwn­ ska rjesenja za nas hrvatski prost or i s ire. Keywords: .ie; concept; dinarida; dinarides; geol; geotectonics; herak; units; zagreb
• Povijest paleobotanickih istrazivanja u Hrvatskoj by Jungwirth, Enio (2010) - 50/2 1 165-171 1 ZAGREB 1997 Povijest paleobotanickih istrazivanja u Hrvatskoj Enio JUNGWIRTH Kljnene rijeCi: paleobolanika. Znacaj paleo­ botanike ocituje se u lome sto proucava sacuvane biljne ostalke (najcesee vegetativne i rasplodne organe - lisee, grancice, plodovc, cesere, pelud, spore i rjede petrifici­ rana stabla) koji su zapravo neznatni dio nekadasnjeg biljnog sv ijeta, a sada ocuvanog u sedimenlima razlicite starost i. Rabeei rezultate paleobotanickih istrazivanja dolazi se do podalaka koji pomazu Keywords: akad; der; die; ettingshausen; flora; geol; istrazivanja; jos; kerner; koji; merilaun; paleobotanickih; rad; razdoblje; sakac; unger; von; wien; wiss; zagreb; znan
• The Development of Croatian Geoscience as Reflected by the Study of Dinaridic Ophiolites by Pamić, Jakob (2010) - He included sedimentary rocks surrounding ophiolites into the Jurassic and Cretaceous and was or the op inion that the zone of igneous rocks represents only a facies within the flysch formations (PILAR , 1882, p. 5 1). The Development of Croatian Geoscience as Reflected by the Study of Dinaridic Ophiolites Jakob PAMIC Key words: Dinaridic ophiolites, Genetically rela ted sedimentary fo rmations, Flysch period, Geosyncline period, Plate tectonics. Keywords: age; cretaceous; croatian; data; early; formation; geol; geology; geoscience; graywacke; ideas; jurassic; majer; map; melange; new; ophiolites; pamic; parts; period; rocks; shale; time; ultramafic; zagreb; zone
• Upper Palaeozoic Fossils from Clastic Sedimentary Rocks in the Gorski Kotar Region by Sremac, Jasenka; Aljinović, Dunja (2010) - sp. c-p • - 5B Anthracoporella spectabilis PIA c-p • • • • 59 Gyroporella likana KOCHANSKY - DEVIDE c, • • 60 GyroporeJfa constricta KOCHANSKY - DEVIDE c, • • • 61 Gyroporelfa microporosa EN DO P • 62 Gyroporella sp. C 2 - P • 67 Paraepimastopora kanumai EN DO C 2 -P • 6B Atractyliopsis carnica E. FLUGEL p, • • ? Keywords: age; brijeg; carboniferous; clastic; gorski; kochansky; kosmacev; kotar; kriz; mrzla; pebbles; permian; rocks; taxa; upper; zagreb
• Upper Triassic Biostratigraphy and Algae from Žumberak (Croatia) by Grgasović, Tonći (2010) - Fossil content: Besides frequent fragments and scarce whole skeletons of the dasyclad alga C/ypeina besici PANTIC (PI. II. Fossil content: Some foraminifera continue iIllO this zone, including: Au/oforfus fl·ieelli (KRISTAN­ TOLLMANN) (PI. II , Fi g. I pars) , Au/olorills lellllis (KRIST AN) and the index species Auloforllls sinllosus WEYNSCHENK (PI. II, Fig. 1 pars), which is thc most 203 numerous. Keywords: algae; arc; besici; branches; fig; figs; flugel; geol; gumbel; pantic; pars; pia; range; section; slide; sokac; species; thallus; triassic; und; zagreb; zone; zumberak
• Review of the Results of Morphometric and Morphogenetic Analyses of Early Pleistocene Micromammals and Upper Pleistocene Cave Bears in Croatia by Jambrešić, Gordana (2010) - The Early Pleistocene age of the bone-breccias discovered along the Adriatic coast was confirmed by the morphogenetic analy ses of micromammals, with reference to geochronolog ically important arvi­ col ids: the fauna fro m Razvode ncar Knin comprises arvieolids char­ acteristic of the Lower Early Pleistocene, the fauna from Tatinja dra­ ga near Karlobag comprises species typical for the Middle Early Pl eistocene, while the fauna from Podumci ncar UncSic is of La te Early Pleistocene age. At the same time the metrical data and molar morphotypes of the genus Lagurlls (Fig. 2), as well as the genus Pliol1lYs (ri g. 3) indicate that the fauna from Razvode (Lower Early Pleistocene) is older than the fa una from Tatinja dra­ ga (M iddle Early Pleistocene), which is somewhat older than the fauna from Podumci (Late Early Pleis­ tocene) (Table 3; PAUNOVIC & RABEDER, 1996). Keywords: age; cave; croatia; early; fauna; fig; malez; paunovic; pecina; pleistocene; podumci; rabeder; results; riss; tatinja; vindija; zagreb
• Bibliography of Professor Milan Herak = Bibliografija Profesora Milana Heraka by *, * (2010) - Min. GeoL Palaeont, (Abh.), (B), 88, 107- 135, Sluttgart 2) HERAK , M. (1944): Sto je paleobiologija?- Priro­ da, 34n- 10, 11 2- 116, Zagreb. 3) HERAK , M. (1944): lz povijesl zavod, 3, 160- 170, Zagreb. 4) HERAK, M. ( 1944): Otkrice krapinskog pracov­ jeka.- Znanje i radost Hrv. Keywords: akad; beograd; cds; der; des; geol; geologija; herak; hrv; istraz; izd; jugos; karst; knjiga; krsa; new; prir; reg; sarajevo; sci; vjesnik; von; water; york; zagreb; zavod; znan
• Professor Milan Herak - on the Occasion of His 80th Birthday by Gušić, Ivan; Kranjec, Velimir (2010) - Despite the fact that, at that time, Abel's palaeobiology was based on neolamarkism, Professor Herak was not inDu- I Department of Geology and Palaeonto logy, Fac ulty of Sciences, University of Zag reb, Ul. In 1952 Professor Hcrak was appointed assistant professor of the then Technical Faculty, In hi s notes Professor Herak states that it was not an easy decision for him j because he had planned his future with the fac­ ulty of Science, However, this employment was very useful for geosciences, as very soon Herak founded the independent D epartme nt for Geology and Palaeonto­ logy. Keywords: book; courses; faculty; geology; herak; professor; sciences; zagreb
• Academician Milan Herak's Main Contribution to Palaeontology by Sokač, Branko; Bajraktarević, Zlatan; Jurišić-Polšak, Zlata (2010) - This paper was presented at the scientific meeting dedicated to the 80th anniversary of the life of Professor Milan Herak, held on March 5th, 1997 in Zagreb 144 of their phy logeny and pointed out the recapitulation of some ontogenetic stages which are probably analogous to phylogenetic stages. KOCI-IANSKY-DEVIDE, V. & HERAK , M. (1960): see # 44 in Bibliography of Professor Milan Herak (this Vol., p.127-135). Keywords: algae; bibliography; fossil; genus; herak; milan; milan herak; p.127; pro­; research; species; vol; zagreb
• Foreword - Uvodna riječ by Hernitz, Zvonimir (2010) - Oeito je cia je prezenta­ cija Ll lOm smislu poslignlltih rezultata oel velikog znacenja za nasl! zemljll. Geolog ia Croatica omoguccno je tiskanje II tom znanslvcnom easopisu. Keywords: economic; exploration; ina; istrazivanja; papers; petroleum; prof; skupa; symposium; zagreb
• Production Characteristics and Reservoir Quality at the Ivanić Oil Field (Croatia) Predicted by Machine Learning System by Hernitz, Zvonimir; Đureković, Miro; Crnički, Josip (2010) - Well no. 11 13 7 12 - 24 27 - 28 29 -- 15 - 30 time (year) 2 4POR > 21.7 1 2 Fig.4 Hydrocarbon produc­ tion rate - good produ­ cers. 240 injector-well section p roduction group boundary oil/Woter contact c ontrolwetl • producers-group I • producers-group II °CI =======5;OO~ ....... 'OOOlm) Number of wells Number of corTeet Reliability learn ing testing answers (%) 25 5 5 100.0 22 8 7 85.5 19 11 8 72.7 16 14 10 7 1.4 Table 3 Reliability of well category prediction (phase 2). Re liability o f the decision tree ana lysis was tes ted on fiv e wel ls Numbcr of wells Number of corrcct Reliability IC311ling testing answers (%) 10 5 2 40.0 15 5 3 60.0 20 5 4 80.0 25 5 4 80.0 Table 5 Reliability of well category prediction (p hase 4). Keywords: depositional; learning; machine; number; oil; phase; production; reservoir; system; table; wells; zagreb
• Geološko-ekonomski esej: " ... koordinirani napori svih zainteresiranih subjekata svjesnih sebe, svojih interesa, svojih mogućnosti i svoje odgovornosti..." (PLETIKAPIĆ, 1988) by Šimon, Jožef (2010) - Otud nedoumice upravljaca, u vre­ mcnu u kojem je jos moguc izbor izmedu prihvacanja idejc i njcna da ljnjcga ignoriranja . Tako se, na primjer, cini da jc dovoljno j asno cia u slozenom procesu koji u scb i saclrzava vise naprecillj ueih ciklusa, prioritcl u naporillla za njihovo nastavljanjc imaju ciklusi najblizi konacnom cilju . Keywords: cia; gas; iii; ina; istrazivanja; kao; koji; mineralnih; nafte; neto; oil; otkrivanja; pletikapic; plina; pod; pri; procesa; rizika; sirovina; sve; svih; tzv; ulaganja; vrijednosti; zagreb; zaliha; zbog
• gc-391 by None (None) - 111 these sediments o il was found: a) in the calcareous component in fi ssures of more gen- erations; b) in sand lcnses o f smal l dimensions; c) in sand layers of large dimens ions; d) in rock mirrors; e) in fractures and fissures a long fau lts; t) in cres ts of brachi anticli ne axes. Oi l may ha ve migrated int o thin sandstone layers, ri ssures formed during men­ tioned oroge ni c phases and, what is mos t import an t, in to the ax ial c res ts o r brach i antic line (BOS KO V iVlasarykova 24, Zagreb, Croalia. Keywords: boskov; oil; sava; zagreb
• gc-402 by None (None) - Ako k lome dodamo da jc osob­ no bila menlor cliplomskih raclova vise od 120-orici stu­ clcnata i stuclentica, od kojih su mllogi poslali sudionici, a ncmali braj i nos itclji izradc OGK Hrvatskc, kao i cia sc vcl iki clio njez inih el iplol11anada zaposl io II Nalta­ plinu, za kojega se zna SIO znaci u gospodarstvu Hrvatskc, onda jc prava rijcc da jc Iljcz ino djelovanje na gClleracije hrvalskih geologa bilo zaista nCl11jcrijivo Ncdclu, koja jc jos dok jc bila akt ivna, postala na nasem fakultctu legendom za geologijll i geolosko kartiranje). Keywords: bila; cia; devlde; nedela; zagreb
• gc-403 by None (None) - Simpozij 1nclu strija nemct ala u obnovi i razyoju Repub like Hrvatske, Zbornik rado­ va, Centar za istrazivanje i razvoj nemetala, 76-84, Zagreb. godine na dllznosti je prcdstojnika Zavoda za mincralne sirovine. Keywords: eugen; godine; krkalo; radova; zagreb
• Dr. Teofil Slišković by Gušić, Ivan (2010) - muzeja B. i H., Prir. nauke, (N.S.), 22, 19-26, Sarajevo, 1983. muzeja B. i H., Prir. nauke, (N.S.), 29, 5-9, Sarajevo, 1990. Keywords: acad; bosne; cons; geol; glasnik; hercegovine; malez; mirko; muzeja; n.s; naslaga; nauke; prir; sarajevo; sci; slišković; teofil; yougosl; zagreb; zemalj
• Mr. Drago Savić by Milanović, Momčilo (2010) - Objavio je sam ili u koautorstvu 25 radova. ŠUŠNJAR, Milan, BUKOVAC, Josip & SAVIĆ, Drago (1967):Paleografski odnosi nakon taloženja anizičkih naslaga u području južne Like. - Geol. Keywords: drago; geol; zagreb
• Ozren Lukić by Kuhta, Mladen (2010) - Geologia Croatica 45 Za sve što je učinio u svom i ovako kratkom životu iskrena mu hvala i Selina izrazio je župnik don Tomislav Baričević. Keywords: duž; godine; istraživanja; njegov; planine; speleološko; sve; zagreb
• In memoriam Professor Vladimir Jurak (1942-2010) by Benac, Čedomir; Mihalić, Snježana; Novosel, Tomo (2011) - In Memoriam Professor Vladimir JURAK (1942–2010) Geologia Croatica 277 BENAC, Č., JURAK, V. & OŠTRIĆ, M. (2005): Qualitative Assessment of Geohazard in Rječina Valley.− Geophysical Research Abstracts, 7, 08943, 1−6. Edizioni Universita di Trieste, 296−298. PETRAŠ, J. JURAK, V. & GAJSKI, D. (2001): Istraživanje ekscesivne erozije na golim fl išnim padinama Keywords: eds; engineering; geology; jugoslavenski; jurak; magdalenić; professor; radova; zagreb; zbornik
• In memoriam Professor Stjepan Šćavničar (1923-2011) by Bermanec, Vladimir (2011) - umjet., 41), 269–275. MARCI, V., MEĐIMOREC, S. & ŠĆAVNIČAR, S. (1975): Žilne pojave klorita u jugozapadnom dijelu Psunja SFRJ (Predavanja), 2, 319–334, Zagreb. ŠĆAVNIČAR, S., MEĐIMOREC, S. & ŠĆAVNIČAR, B. (1975): Pum- pellyite in the magmatic rocks of Komiža.– Keywords: acta; bermanec; croatian; crystal; geol; jugosl; structure; tibljaš; zagreb; šćavničar
• First record of Acanthuridae (surgeonfish) from the Miocene deposits of the Medvednica Mt. by Tripalo, Kristina; Japundžić, Sanja; Sremac, Jasenka; Bošnjak, Marija (2016) - Special attention was given to those with mesh size of 0.2 and 0.125 mm as these were the fractions where fossil fish teeth were discovered. Fish teeth are particularly common and well preserved reflecting their solid construction. Keywords: acanthuridae; bolca; fish; fossil; medvednica; miocene; tooth; tyler; zagreb
• Milan Herak (1917-2015) by Gušić, Ivan; Juračić, Mladen (2015) - In: Karst, Impor­ tant karst regions of the Northern Hemisphere, M. Herak & V. T. Stringfield, eds., Elsevier, Amsterdam, 25–83. 57. HERAK, M. & STRINGFIELD, V. T. (1972): Historical re­ view of hydrogeologic concepts. HERAK M. (2012): A generalized „southern“ review of the tectogenetic relationships oft he „Dinarides“ and „Alpides“.– Geol. Keywords: acta; akad; croatian; croatica; der; dinarides; edition; geol; geologija; geology; herak; hrv; istraž; izd; jugosl; karst; knjiga; krša; m. herak; milan herak; prir; umjetn; vjesnik; yugoslavia; zagreb; za­; zbornik; znan; školska
• Influence of groundwater quality indicators on nitrate concentrations in the Zagreb aquifer system by Kovač, Zoran; Nakić, Zoran; Pavlić, Krešimir (2017) - Pourbaix diagram for nitrogen species at Zagreb aquifer (background picture modified according to PUIGDOMENECH, 2006; HUSSON, 2013). Histogram of average ORP values at Zagreb aquifer. Keywords: analysis; aquifer; cluster; concentrations; correlation; et al; groundwater; nitrate; no3; orp; system; values; zagreb

• Palaeoecology of the Late Badenian foraminifera and ostracoda from the SW Central Paratethys (Medvednica Mt., Croatia) by Pezelj, Đurđica; Sremac, Jasenka; Sokač, Ana (2008) - O E 1 2 0 1 4 4 2 2 317 310 14 333 311 303 297 300 Table 1 List of identified benthic foraminifera species with their oxic preferences, modes of life and absolute abundance for each standard- ized sample (O – oxic, S – suboxic, D – disoxic, I – infauna, E – epifauna). ZAGREB 2007 Key words: Benthic foraminifera, Ostracoda, Palaeo- ecology, Biostratigraphy, Late Badenian, Medved- nica Mt., Croatia. Keywords: badenian; community; d´orbigny; environment; foraminifera; index; indicators; middle; miocene; number; ostracoda; oxygen; samples; shelf; species; specimens; water
• The relationship between the geochemical and mineralogical characteristics of Calcocambisol, colluvium and recent marine lake sediment of the narrow seashore intertidal zone: a case study from the Veliko Jezero (Mljet Island, Croatia) by Ružičić, Stanko; Durn, Goran; Sondi, Ivan; Mihaljević, Lucija; Ivanić, Maja (2021) - Physico-chemical properties of the analyzed samples All the analyzed samples showed a moderately alkaline reaction (pHH2O), while pHKCl steadily increased from Calcocambisol (7.09) to marine lake sediment (8.17) (Table 1). Similar values of pHH2O and pHKCl were expected in marine lake sediment because it contains pore water with a high NaCl content, which affects the pHH2O measurement (both NaCl and KCl are neutral salts). Keywords: calcocambisol; clay; colluvium; doi; et al; fraction; lake; lake sediment; marine; marine lake; mineral; mljet; samples; sediment; soil; table
• Middle Miocene marine flooding: New 40Ar/39Ar age constraints with integrated biostratigraphy on tuffs from the North Croatian Basin by Marković, Frane; Kuiper, Klaudia; Ćorić, Stjepan; Hajek-Tadesse, Valentina; Hernitz Kučenjak, Morana; Bakrač, Koraljka; Pezelj, Đurđica; Kovačić, Marijan (2021) - Estimates of the timing of the marine flooding event in the southern part of the Pannonian Basin range from 17 Ma to 15 Ma (HAJEK-TADESSE et al. 2009; PREMEC FUĆEK et al., 2017; HERNITZ KUČENJAK et al., 2018; PAVELIĆ & KOVAČIĆ, 2018; SANT et al., 2018, 2019; MANDIC et al 2019a, BRLEK et al., 2020) and are a matter of debate. The dura- tion of these phases was diachronous across the basin (MA- TENCO & RADIVOJEVIĆ, 2012; BALÁZS et al., 2016). Keywords: 40ar/39ar; age; badenian; basin; central; croatian; doi; environment; et al; fig; foraminifera; geol; layer; laz; locality; mandic; marine; middle; miocene; ncb; nježić; pannonian; paratethys; samples; tuff; zone; čučerje
• Palaeomagnetic Results from the Sarmatian/Pannonian Boundary in North-Eastern Croatia (Vranovi? Section, Našice Quarry) by Vasiliev, Iuliana; Bakrač, Koraljka; Kovačić, Marijan; Abdoul Aziz, Hayfaa; Krijgsman, Wout (2008) - The basin formed in the Early Miocene, as a consequence of continental collision and subduction of the European Plate under the Apulian Plate (TARI et al., 1992; HOR- Fig. 1 Location of the studied area: (a) Pannonian Basin; (b) Study area; (c) Geological sketch map after KOROLIJA & JAMIČIĆ, 1988. The post-rift phase of basin formation (Upper Badenian to recent) is characterized by subsidence due to lithos- pheric cooling, with occasional inversions of the basin generated by intraplate stress that affected the entire Pannonian Basin (HORVÁTH & CLOETINGH, 1996). Keywords: age; basin; boundary; et al; field; fig; miocene; pannonian; paratethys; samples; sarmatian; section; vranović
• The contribution of geochemical and mineralogical characterization of iron slags in provenance studies in the Podravina region, NE Croatia by Brenko, Tomislav; Karavidović, Tena; Borojević Šoštarić, Sibila; Sekelj Ivančan, Tajana (2022) - A) Map of the study area with locations of iron slags and iron ores used in this study. The contribution of geochemical and mineralogical characterization of iron slags in provenance studies in the Podravina region, NE Croatia Tomislav Brenko1,*, Tena Karavidović2, Sibila Borojević Šoštarić1 and Tajana Sekelj Ivančan2 1 University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Department of Mineralogy, Petrology and Mineral Resources, Pierottijeva 6, 10 000 Zagreb, Croatia; (*corresponding author: tomislav.brenko@rgn.unizg.hr) 2 The Institute of Archaeology, Jurjevska ulica 15, 10 000 Zagreb, Croatia doi: 10.4154/gc.2022.11 Abstract Archaeological excavations in the Podravina region led to discovery of sites with traces of bloom- ery iron production during Late Antiquity and the Early Middle Ages. Keywords: + +; bog; bog iron; doi; elements; et al; geochemical; hlebine; iron; iron ores; iron slags; ore; ores; samples; site; slags; trace; virje
• Evidence and mineralogical and physico-chemical properties of chernozem and chernozem-like soils in Croatia by Galović, Lidija; Husnjak, Stjepan; Šorša, Ajka; Martinčević Lazar, Jasmina (2023) - Soil profile P-3 is characterised by the structure of the Ap- A-AC-C profile, where the surface part of the A horizon is anthro- pogenic down to a depth of about 42 cm and represents the arable horizon. The area with a dominant presence of chernozem, with occasional occurrences of rendzina on the loess; b) Locations of soil profiles P-3, P-6 and P-10. Keywords: chernozem; clay; composition; content; croatia; depth; doi; fraction; galović; grains; horizon; loess; minerals; muscovite; p-10; p-3; p-6; profile; samples; soil
• Uranium Minerals in the Radlovac Series Metasediments at Mt. Papuk, Croatia by Šćavničar, Stjepan; Bermanec, Vladimir; Kniewald, Goran; Barišić, Delko; Oreščanin, Višnja (2008) - 1 University of Zagreb, Faculty of Science, Institute of Mineralogy and Petrology, Horvatovac bb, HR-10000 Zagreb, Croatia; e-mail: vberman@public.carnet.hr 2 Rudjer Bošković Institute, Department of Marine and Environmen- tal Research, POB 180, HR-10002 Zagreb, Croatia Abstract Applying a combination of different methods – X-ray diffraction, scanning electron microscopy, gamma-spectroscopy and X-ray spec- troscopy, a suite of uranium minerals, meta-torbernite, meta-uranos- pinite and meta-zeunerite was identified in metasediments of the Rad- lovac series at the Mt. Papuk area, Croatia. The powder pattern of the chloritoid minerals presents a major difficulty in the identification proc- ess of uranium minerals present in the samples. Keywords: activities; fig; meta; minerals; papuk; ppm; radlovac; samples; series; uranium
• The influence of weathering and pedogenesis on the geochemical record of Miocene marls and Plio-Quaternary sediments, Medvednica Mt., Croatia by Gverić, Zvonka; Tomašić, Nenad; Durn, Goran; Rubinić, Vedran (2024) - 0.0005 - H2 250* 22 2 0.0006 0.0183 * marks PlQ sediment samples b.d.l. 5. CONCLUSIONS The results of this study show that, in general, there is a good correlation between the geochemical and mineralogical weathering signatures in the parent materials, weathered materials and soil samples, which were analyzed in the foothill area of Medvednica Mt. Keywords: chemical; clay; croatia; doi; elements; et al; marl; material; mineralogy; minerals; miocene; parent; pedogenesis; plq; profiles; samples; sections; sediments; soil; soil samples; weathering
• Tracing the origin of raw materials used for the production of ancient ceramics: a case study of multi-period archaeological sites in the Turopolje area (Continental Croatia) by Neral, Natali; Kudelić, Andreja; Maričić, Ana; Mileusnić, Marta (2024) - According to previous studies and considerations (KREITER, 2007; ALBERO SANTACREU, 2014), the choice of pottery raw materials, especially temper, can be culturally conditioned, which partly rejects environmental and techno- functional reasons. Therefore, to enhance the understanding of raw material selection processes and ensure a more robust dataset for considering their provenance and distribution over time, the research incorporates geochemical data from ceramic sherds and clay samples from the nearby Kurilovec-Belinščica site (Early Bronze Age and Middle/Late Bronze Age). Keywords: + +; age; bronze; ce ra; ceramics; clay; clayey; ic s; m ic; m s; materials; r +; ra m; s kb; samples
• Strontium Isotopic Stratigraphy of the Miocene Adana Basin (S. Anatolia) and its Geological Implications by Akinci, Ahmet Can (2025) - et al., 2012), which is significantly greater than the mixing time of the ocean (approximately 103 years). The carbonate rocks compiled for Sr isotope analysis from the Late Miocene carbonates (Figs. Keywords: adana; adana basin; age; alteration; analysis; basin; carbonate; cingöz; et al; fig; formation; güvenç; implications; isotope; isotopic; kaplankaya; karaisalı; kuzgun; marine; mediterranean; messinian; miocene; samples; sediments; stratigraphy; strontium; turkey; unit; ünlügenç
• Deciphering the pedo-sedimentary complex of eastern Adriatic coast: Case study from Privlaka, Croatia by Ružičić, Stanko; Galović, Lidija; Beerten, Koen; Hećej, Nina; Martinčević Lazar, Jasmina; Gajić, Rodoljub; Husnjak, Stjepan; Poch, Rosa Maria; Pandurov, Mihajlo; Stejić, Petar; Pjanić, Ajka (2025) - In order to determine the age of carbonate grains, micropalaeontological analyses were carried out. In addition to the reported lithic particles, serpentinite particles (specific density 2.6 g cm-1) plastered with quartz grains are found in the oldest 18-1 horizons (Fig. 6g). Keywords: age; carbonate; complex; concretions; croatia; dose; et al; fig; grains; horizon; layer; loess; material; mineral; palaeosol; pedo; privlaka; profile; quartz; samples; sand; table; unit
• Characteristics, origin and geoarchaeological significance of carbonate concretions from the early Bronze Age locality „Orovački vinogradi“, (Bjelovar, Croatia) by Barudžija, Uroš; Jakovljević, Goran; Aljinović, Dunja; Brčić, Vlatko; Tadej, Neven (2010) - 4. RESULTS During the archaeological excavation we examined a 7 m thick, undisturbed, vertical succession, consisting of sand and sandstone beds and horizons with white concretions. barudzija.indd 323 � AB STRA CT “White horizon” archaeological units consisting of carbonate concretions occur in the archaeological settlement of “Orovački vinogradi”, located near Bjelovar (NW Croatia). Keywords: carbonate; concretions; horizon; orovački; samples; sand; settlement; units; vinogradi
• Zeolitization of Tuffaceous Rocks in the Keşan Region, Thrace, Turkey by Esenli, Fahri; Uz, Bektas; Suner, Fikret; Esenli, Vildan; Ece, Ö. Işık; Kumbasar, Işık (2010) - These minerals are generally the major components of rock samples according to the XRD patterns (Fig. 2). Powdered rock samples have been fused using LiBO2 and the resulting glass disks have been analyzed in the research laboratory of Turkish Glass Inc. Keywords: analcime; clinoptilolite; fig; heulandite; keşan; minerals; mordenite; rocks; samples; thrace; zeolites
• Recent Sediments of Makirina Cove (Northern Dalmatia, Croatia): Their Origin Viewed Through a Multidisciplinary Approach by Šparica, Marko; Koch, Georg; Belak, Mirko; Miko, Slobodan; Šparica-Miko, Martina; Viličić, Damir; Dolenec, Tadej; Bergant, Stanislav; Lojen, Sonja; Vreča, Polona; Dolenec, Matej; Ogrinc, Nives; Ibrahimpašić, Haris (2010) - The bio- availability of Se in Makirina Cove sediments based on the concentration difference of Se extracted with 7 mol HNO3 and total Se (HF–HCl–HNO3) implies a range of 40–60%. According to the results obtained from the applied methods, the features of Makirina sediments strongly reflect the given depositional conditions within this restricted, stressed, shal- low-marine environment where these organic-rich sediments originate, and may therefore serve as a calibration standard in further investiga- tions. Keywords: 0–5; 20–25; 58/1; adriatic; aom; bay; calcite; carbon; carbonate; composition; conditions; cove; croatia; distribution; environments; et al; fig; geologia; isotopic; light; makirina; makirina cove; marine; matter; mean; minerals; northern; plate; ppm; preservation; samples; sea; sediments; shore; silt; table; values; vulgata; water; δ13c
• Discriminant Function Analysis of Miocene Volcaniclastic Rocks from North-Western Croatia Based on Geochemical Data by Tibljaš, Darko; Loparić, Vanja; Belak, Mirko (2010) - E B9 B B E K B25 B B E K B31 B B E K B35 B B E K B36 B B E K B40 B B E K B42 B B K E B43 B B E K B46* B K B E B51 B B E K KREM (Poljanska Luka) B B E K SIVA (Poljanska Luka) B B E K T-6-94-4B (Cerovec) E E B K T-5-93-17 (TrliËno) E E B K T-5-93-21 (Hromec) E E B K T-5-93-18 (Hromec) E E B K T-6-93-17E (Donje Jesenje) E E B K T-7-90-K2 (Donje Jesenje) E E B K T-790-K5 (Donje Jesenje) E E B K T-7-90-K18 (Donje Jesenje) E E B K T-7-90-K22 (Donje Jesenje) E E B K T-7-90-K27 (Donje Jesenje) E E B K T-7-90-K27G (Donje Jesenje) E E B K T-7-90-15 (Donje Jesenje) E E B K T-7-90-30 (Gornje Jesenje) E E B K T-7-90-33 (Gornje Jesenje) E E B K T-4-98-1 (Gornje Jesenje) E E B K T-7-90-2 (Cerje Jesensko) E E B K T-7-90-4B (Cerje Jesensko) E E B K T-7-90-7 (Cerje Jesensko) E E B K T-7-90-8 (Cerje Jesensko) E E B K T-7-90-57 (Jamno) E E B K T-7-90-62 (Jamno) E E B K T-6-93-14 (Jamno) E E B K LEPOGLAVA E E B K T-4-99-8 (Vuglovec) E E B K T-4-99-9 (Vuglovec) E E B K T-4-99-10 (Vuglovec) E E B K T-4-99-11 (Vuglovec) E E B K PODRUTE E E B K HMPM7110 (Jesenje) - E B K T-7-90-©1 (©aπa) - E B K T-3-90-1 (Lapornica) - E B K ©EPRUN3 - E B K HMPM7113 (Moæenec) - E B K HMPM7115 (Moæenec) - E B K T-4-99-3 (Moæenec) - E B K T-4-99-7 (Moæenec) - E B K T-4-99-5S (Moæenec) - E B K T-4-99-2A (Moæenec) - E B K T-4-99-4 (Moæenec) - E B K VHK500 (Kalnik - Drenovec) - K B E T-5-99-1 (Kalnik - Knezov jarak) - E B K KALNIK (Knezov jarak) - E B K VHK227 (Kalnik - Knezov jarak) - E B K Table 3 Classification of samples on the ba- sis of discriminant function analysis. In the north-western part of Croatia, belonging to the South Pannonian Basin, numerous small occurrences of Miocene volcanic and volcaniclastic rocks have been discovered (©IMUNI∆ et al., 1981; ANI»I∆ & JU- RI©A, 1985; PAMI∆, 1997 and references therein). Keywords: age; b k; e b; e e; rocks; samples
• Distribution of Iron and Manganese in Terra Rossa from Istria and its Genetic Implications by Durn, Goran; Slovenec, Dragutin; Čović, Marta (2001) - ZAGREB 2001 Key words: Terra rossa, Iron, Manganese, Iron oxi- des, Istria, Croatia. Limited variation of selected Fe oxide characteristics in analysed samples indicates the specific pedogenic environment in which terra rossa is formed. Keywords: clay; haematite; iron; manganese; oxides; rossa; samples; schwertmann; soil; terra; terra rossa
• Strontium Dependence of the Lattice Constants of Barites from the Kreševo Area in Central Bosnia (Bosnia and Herzegovina) by Slovenec, Dragutin; Šiftar, Dubravko A.; Jakšić, Milko A.; Jurković, Ivan (2010) - Quartz is a very suitable mineral and often occurcs in barite ore samples. However, diffraction lines oj other samples were not so well-defined, and the lines or samplc 7 were sub­ stantially broadened in rclation to synthet ic BaS04 (Fig. Ic). Keywords: barite; bas04; data; diffraction; fig; ing; kresevo; line; method; mole; parameters; quartz; samples; spacing; synthetic; unit; values; xrd
• Venezuelan sandstone caves: a new view on their genesis, hydrogeology and speleothems by Aubrecht, Roman; Lánczos, Tomáš; Šmída, Branislav; Brewer-Carías, Charles; Mayoral, Federico; Schlögl, Ján; Audy, Marek; Vlček, Lukáš; Kováčik, Lubomír; Gregor, Miloš (2008) - Keywor ds: speleology, tepuis, Venzuela, sandstone caves, siliceous speleothems, microbialites, cyanobacteria, stroma- tolites, hydrogeochemistry. Alternative views on the genesis of sandstone caves are presented here, based on geological, geomorphological, hy- drogeochemical and speleological observations. Keywords: beds; brewer; caves; charles; croatica; cueva; dissolution; formation; genesis; geologia; lithifi; roraima; samples; sandstone; speleothems; water
• gc-39 by None (None) - Geo.Cro.2-3-61-KB.pdf 379 � Borna Lužar-Oberiter1, Snježana Mikulčić Pavlaković2, Marta Crnjaković2 and Ljubomir Babić1 AB STRA CT The composition of beach sands from the Islands of Rab and Susak (northern Adriatic) has been studied in order to determine how individual beaches are supplied with detritus. Keywor ds: beach sands, sediment supply, framework composition, heavy minerals, Rab, Susak, Croatia 1 Department of Geology, Faculty of Science, University of Zagreb, Horvatovac 102a, 10000 Zagreb, Croatia; (bluzar@geol.pmf.hr) 2 Croatian Natural History Museum, Demetrova 1, 10000 Zagreb, Croatia Variable sources of beach sands of north Adriatic islands: examples from Rab and Susak Geologia Croatica 61/2–3 379–384 4 Figs. Keywords: beach; beaches; carbonate; island; mineral; pleistocene; rab; samples; sands; susak
• gc-43 by None (None) - Chloritoid schists (samples 2 and 3) are dark grey, fi ne- grained metamorphic rocks with well observed schistosity defi ned by their dominant grano-lepidoblastic matrix (Fig. 2B). Bisevac.indd 63 � Vanja Biševac1, Dražen Balen1, Darko Tibljaš1 and Darko Španić2 AB STRA CT Samples from the Radlovac metamorphic complex, together with others from the overlying sedimentary rocks, and parts of Psunj metamorphic complex beneath it were studied in order to better constrain metamorphic conditions that have prevailed in the area. Keywords: + +; chlorite; complex; kübler; low; pamić; quartz; samples; árkai
• gc-463 by None (None) - Magnetite is commonly partly altered to hematite, and in most rock samples these minerals occur together. In some samples relict fragments of clinopyroxenes are observed, and in sample l only their contours containing secondary minerals are preserved. Keywords: alteration; chlorite; composition; diabase; epidote; fig; kamešnica; minerals; rocks; samples; spilites; texture
• Mineralogical and geomicrobiological investigation of phosphorite from Ervenik, Croatia by Bermanec, Vladimir; Posilović, Hrvoje; Žigovečki Gobac, Željka; Hrenović, Jasna; Mikac, Nevenka; Kniewald, Goran (2011) - By calculating unit cell parameters, it is possible to conclude that these are apatite group minerals (Ca5(PO4)3X, X=F, OH, Cl), having unit cell parameters comparable to fl uorapatite and hydroxylapatite. A substantial number of hyphae were observed on the surface of phosphate minerals, in addition to saprophytic bacteria and bacterial spores. Keywords: apatite; bacteria; crandallite; croatia; minerals; phosphate; phosphorite; samples
• Geochemical discrimination of Early Palaeogene bauxites in Croatia by Kovačević Galović, Erli; Ilijanić, Nikolina; Peh, Zoran; Miko, Slobodan; Hasan, Ozren (2011) - Geochemically, it can be understood as IST bauxites being enriched in K2O–TiO2 and depleted in P2O5 with regards to NDA and CDA bauxites, and vice versa. In con- trast, IST and NAI bauxite groups of the Istrian Karst Adri- atic unit and northern part of the High Karst Dinaridic unit, respectively, contain below-average Cr content. Keywords: adcp; adriatic; bauxites; carbonate; cda; conditions; dfm; discriminant; element; groups; ist; karst; major; nai; nda; palaeogene; samples; trace
• Late Pleistocene climate history of the Baranja loess plateau – evidence from the Zmajevac loess-paleosol section (northeastern Croatia) by Banak, Adriano; Mandić, Oleg; Kovačić, Marijan; Pavelić, Davor (2012) - MS values are in the expected range, especially in loess horizons. Finally open habitat representatives likely dominate the section with mean abundance of 66.81% and peak in L5 loess horizon (71.4%). Keywords: assemblage; climate; columella; croatia; et al; fig; helicopsis; horizon; late; loess; mollusc; palaeosol; pleistocene; samples; section; zmajevac
• Contamination of seabed sediments around a shipyard in the Adriatic Sea (Ugljan island) by Fajković, Hana; Prohić, Esad; Abramović, Daniela (2013) - CEULEMANS, M., SLAETS, S. & ADAMS, F. (1998): Speciation of organotin in environmental sediment samples.– Talanta, 46, 395– 405.  Contamination of seabed sediments around a shipyard in the Adriatic Sea (Ugljan island) Keywords: doi; elements; results; samples; sand; sediment; shipyard; values
• Distribution of copper and zinc in the soil of an industrial zone in the city of Garešnica, Croatia by Medunić, Gordana; Tomašić, Nenad; Balen, Dražen; Oreščanin, Višnja; Prohić, Esad; Kampić, Štefica; Ivanišević, Danijel (2009) - In Figure 1 numbers 1–15 is soil samples collected in the vicinity of the B and CP factories, constituting a total of 30 samples. Ur- ban and control soil samples were all rather similar in their visual appearance, i.e. texture. Keywords: copper; correlation; doi; et al; group; metal; ppm; samples; signifi; soil; values
• Geochemistry of the Görcsöny Ridge amphibolites (Tisza Unit, SW Hungary) and its geodynamic consequences by Toth, Tivadar M. (2014) - Unit UU UU UU UU UU UU UU UU UU UU UU UU Sample B2-680 B2-681 B2-699 B2-701 B2-702 B2-703 B2-704 B2-706 B2-707 B2-708 B2-709 B2-711 Depth 827 m 829 m 846 m 850 m 853 m 854 m 854 m 857 m 859 m 861 m 864 m 866 m SiO2 49.09 48.88 47.22 46.24 47.13 47.49 50.43 48.15 46.67 47.49 46.48 44.73 TiO2 3.17 3.29 2.62 2.75 3.81 4.26 2.92 3.01 3.14 2.86 3.34 3.76 Al2O3 13.42 14.08 11.65 12.80 14.46 14.83 13.81 14.48 14.34 14.59 13.92 14.70 Fe2O3 tot 11.78 11.65 13.49 14.33 12.14 14.19 13.69 13.47 13.84 12.74 13.22 15.85 MnO 0.30 0.19 0.21 0.23 0.18 0.23 0.23 0.20 0.18 0.18 0.18 0.23 MgO 6.25 6.45 8.75 7.63 4.31 4.76 3.51 6.58 4.85 6.59 6.19 5.36 CaO 10.36 9.67 11.27 10.64 11.01 8.61 8.72 8.32 10.94 9.51 10.67 8.67 Na2O 3.10 3.18 2.51 2.61 4.13 4.15 5.20 3.69 3.25 3.55 3.07 3.34 K2O 1.15 1.32 0.82 0.99 0.57 0.87 0.50 1.17 1.24 0.85 1.21 0.43 P2O5 0.38 0.39 0.39 0.33 0.39 0.46 0.92 0.35 0.47 0.32 0.45 0.66 lOI 1.22 1.32 1.19 1.06 1.68 0.62 0.36 0.89 1.02 1.01 1.17 2.68 Total 100.21 100.40 100.12 99.61 99.81 100.45 100.29 100.32 99.93 99.72 99.89 100.41 Cr 93 94 188 132 14 9 15 92 43 101 147 80 Ni 79 62 97 89 15 11 1 65 30 66 65 31 v 398 428 342 396 403 421 174 372 397 378 409 381 Rb 80 81 30 37 13 25 2 32 54 21 41 22 Sr 433 492 235 305 450 511 416 553 429 430 426 491 Ba 171 263 165 148 111 137 92 254 215 138 226 70 Ga 18 21 15 19 26 25 24 22 22 21 21 33 Nb 31 31 24 25 32 39 65 29 34 29 37 45 Y 31 31 23 27 29 34 61 27 36 28 33 41 Zr 186 190 148 141 184 223 400 193 213 174 206 238 Unit lU lU lU lU lU lU lU lU lU lU lU lU Sample B2-803 B2-804 B2-810 B2-811 B2-816 B2-828 B2-832 B2-833 B2-889 B2-907 B2-911 B2-913 Depth 1020 m 1022 m 1035 m 1036 m 1044 m 1062 m 1066 m 1067 m 1128 m 1150 m 1152 m 1153 m SiO2 55.59 50.07 49.95 49.84 43.65 50.06 47.87 50.43 48.98 49.74 47.45 48.78 TiO2 1.40 2.10 3.83 0.86 3.62 2.94 2.68 2.72 2.11 2.82 3.07 3.75 Al2O3 18.15 14.78 14.16 10.55 10.68 11.14 14.43 14.68 15.44 17.37 16.24 14.27 Fe2O3 tot 8.27 11.69 14.21 12.25 14.74 13.22 12.03 12.59 12.99 11.75 12.24 13.75 MnO 0.06 0.15 0.19 0.18 0.15 0.17 0.16 0.19 0.21 0.19 0.22 0.27 MgO 4.49 8.44 4.73 12.87 8.03 9.62 6.66 6.74 7.38 3.64 5.25 5.28 CaO 3.89 7.55 8.31 10.04 14.10 9.08 8.12 8.27 9.02 10.87 11.23 10.08 Na2O 3.20 0.68 1.31 0.83 0.89 0.88 2.23 2.27 1.39 0.99 1.09 1.94 K2O 1.74 2.39 1.59 0.97 0.78 1.29 1.80 0.97 1.02 0.88 1.45 1.04 P2O5 0.18 0.24 0.76 0.10 0.75 0.39 0.37 0.40 0.28 0.48 0.69 0.21 lOI 3.05 2.26 1.25 1.86 2.27 1.65 3.45 1.07 1.62 1.29 1.33 0.77 Total 100.01 100.35 100.28 100.36 99.65 100.44 99.82 100.34 100.44 100.01 100.25 100.13 Cr 136 349 28 598 483 615 165 149 201 60 86 32 Ni 44 84 25 477 417 188 93 90 74 33 47 6 v 257 298 455 141 283 366 372 328 357 316 382 378 Rb 86 115 97 25 48 73 103 41 45 35 70 28 Sr 269 115 132 35 129 34 173 152 131 282 233 262 Ba 280 236 161 222 78 118 217 125 122 42 105 210 Ga 20 21 29 17 25 18 19 18 24 35 34 24 Nb 19 19 35 8 50 28 33 32 16 37 45 56 Y 21 22 33 19 33 21 32 32 24 38 33 51 Zr 177 130 200 82 308 154 196 192 122 244 219 360 Tivadar M. Tóth: Geochemistry of the Görcsöny Ridge amphibolites (Tisza Unit, SW Hungary) and its geodynamic consequences Geologia Croatica 23 Unit lU lU lU lU lU lU lU lU lU lU lU lU Sample B2-803 B2-804 B2-810 B2-811 B2-816 B2-828 B2-832 B2-833 B2-889 B2-907 B2-911 B2-913 Depth 1020 m 1022 m 1035 m 1036 m 1044 m 1062 m 1066 m 1067 m 1128 m 1150 m 1152 m 1153 m SiO2 55.59 50.07 49.95 49.84 43.65 50.06 47.87 50.43 48.98 49.74 47.45 48.78 TiO2 1.40 2.10 3.83 0.86 3.62 2.94 2.68 2.72 2.11 2.82 3.07 3.75 Al2O3 18.15 14.78 14.16 10.55 10.68 11.14 14.43 14.68 15.44 17.37 16.24 14.27 Fe2O3 tot 8.27 11.69 14.21 12.25 14.74 13.22 12.03 12.59 12.99 11.75 12.24 13.75 MnO 0.06 0.15 0.19 0.18 0.15 0.17 0.16 0.19 0.21 0.19 0.22 0.27 MgO 4.49 8.44 4.73 12.87 8.03 9.62 6.66 6.74 7.38 3.64 5.25 5.28 CaO 3.89 7.55 8.31 10.04 14.10 9.08 8.12 8.27 9.02 10.87 11.23 10.08 Na2O 3.20 0.68 1.31 0.83 0.89 0.88 2.23 2.27 1.39 0.99 1.09 1.94 K2O 1.74 2.39 1.59 0.97 0.78 1.29 1.80 0.97 1.02 0.88 1.45 1.04 P2O5 0.18 0.24 0.76 0.10 0.75 0.39 0.37 0.40 0.28 0.48 0.69 0.21 lOI 3.05 2.26 1.25 1.86 2.27 1.65 3.45 1.07 1.62 1.29 1.33 0.77 Total 100.01 100.35 100.28 100.36 99.65 100.44 99.82 100.34 100.44 100.01 100.25 100.13 on the TAS diagram (LE MAITRE, 1989, Fig. 4), rock samples of UU are plotted close to the alkali basalt field, while those belonging to LU are more differentiated and are subalkali in character (Fig. 4 inset, IRvINE & BARAGAR, 1971). Keywords: amphibolites; biotite; complex; compositions; croatica; evolution; fig; garnet; görcsöny; hungary; n.d; ridge; rocks; samples; tisza; unit
• Geochemical characteristics and genesis of Mačje Jame and Vranjski Potok As-Cu-bearing iron occurrences west and southwest of the town of Busovača, Mid-Bosnian Schist Mountains by Jurković, Ivan; Hrvatović, Hazim (2014) - REE content in the Mačje Jame deposit Table 6a Sample MA-JA MA-JS MA-JP Chemical method MDL FUS-MUS FUS-MUS MDL 4B Average Analyte ppm ppm ppm ppm ppm ppm La 0.050 9.62 56.60 0.1 2.90 23.04 Ce 0.050 20.10 129.00 0.1 6.50 51.87 Pr 0.010 2.48 14.20 0.02 0.95 5.88 Nd 0.050 9.21 43.70 0.3 4.80 19.24 Sm 0.010 3.27 11.70 0.05 2.64 5.87 Eu 0.005 1.28 4.89 0.02 1.98 2.72 Gd 0.010 4.50 13.70 0.05 5.23 7.81 Tb 0.010 1.16 3.41 0.01 1.49 2.02 Dy 0.010 8.90 25.60 0.05 11.43 15.31 Ho 0.010 2.06 5.73 0.02 3.03 3.61 Er 0.010 6.93 18.60 0.03 9.87 11.80 Tm 0.005 1.18 2.98 0.01 1.58 1.91 Yb 0.010 8.23 19.90 0.05 9.85 12.66 Lu 0.002 1.21 2.80 0.01 1.46 1.82 Total 80.13 352.81 63.71 165.55 REE contents in the Vranjski Potok ore deposit Table 6b Sample MDL BOS-09 BOS-10 BOS-12 BOS-13 BOS-15 Average Analyte ppm ppm ppm ppm ppm ppm ppm La 0.10 30.00 57.60 39.80 60.00 13.60 40.02 Ce 0.10 56.30 114.40 68.30 117.10 29.70 77.16 Pr 0.02 5.47 13.67 8.20 13.42 3.41 8.83 Nd 0.30 17.10 51.10 29.60 50.90 12.90 32.32 Sm 0.05 2.82 10.22 4.47 9.80 2.29 5.92 Eu 0.02 0.87 4.56 1.77 3.07 0.92 2.24 Gd 0.05 2.36 8.61 5.59 8.37 1.80 5.35 Method 4B 4B 4B 4B 4B 4B Analyte ppm ppm ppm ppm ppm ppm Ba 1.0 48.00 172.00 165.00 360.00 605.00 Be 1.0 <1.00 <1.00 <1.00 1.00 <1.00 Co 0.2 14.90 17.50 83.20 11.80 5.80 Cs 0.1 0.40 1.80 0.50 3.80 1.40 Ga 0.5 13.00 15.60 5.10 25.40 10.30 Hf 0.1 1.70 1.70 0.10 2.30 2.00 Nb 0.1 7.50 9.70 3.10 22.80 7.70 Rb 0.1 5.80 44.90 13.80 93.60 44.80 Sn 1.0 49.00 54.00 181.00 28.00 16.00 Sr 0.5 8.00 12.30 11.20 13.10 8.40 Ta 0.1 0.60 0.80 0.10 1.30 0.60 Th 0.2 6.60 10.40 0.80 17.00 5.50 U 0.1 1.10 2.80 1.20 3.00 0.80 V 8.0 39.00 55.00 13.00 83.00 38.00 W 0.5 <0.50 3.40 <0.50 3.90 0.90 Zr 0.1 60.50 54.70 5.30 85.60 56.80 Y 0.1 15.20 25.80 46.70 26.30 7.40 Total 271.30 482.40 530.10 781.90 811.40 Trace elements (Mo-Se) in the Vranjski Potok deposit Table 5b Sample MDL BOS-09 BOS-10 BOS-12 BOS-13 BOS-15 Anal. Keywords: content; deposit; jame; mačje; mačje jame; minerals; ore; ore deposit; potok; ppm; ppm ppm; quartz; rocks; samples; table; trace; vranjski; vranjski potok
• Geotechnical properties in relation to grain-size and mineral composition: case study landslide in the Rječina Valley (Croatia) by Benac, Čedomir; Oštrić, Maja; Dugonjić Jovančević, Sanja (2014) - Geotechnical properties in relation to grain-size and mineral composition: The Grohovo landslide case study (Croatia) Geologia Croatica 133 minerals: kaolinite, illite, chlorite, mixed­layer clay miner- als, and in some samples vermiculite (not detected in sample No. 9) and smectite (not detected in sample No. 5­9 and No. 14­16) (IGH, 2000). Phyllosilicates in tested samples are prevalent and are re presented by micaceous minerals, kaolinite, vermiculite, smec tite and chlorite groups, and mixed­layer clay minerals. Zagreb 2014 Geotechnical properties in relation to grain-size and mineral composition: The Grohovo landslide case study (Croatia)  Čedomir Benac1, Maja Oštrić2 and Sanja Dugonjić Jovančević1 1 University of Rijeka, Faculty of Civil Engineering, Radmile Matejčić 3, Rijeka, Croatia 2 Croatian Waters, Department of Rijeka, Đure Šporera 3, Rijeka, Croatia doi: 10.4154/gc.2014.09 The infi ltration of vadose water and increase of inter­particle and inter­aggregate pore water causes swelling of the mont­ mo rillonite and illite groups of clay minerals. Keywords: analysis; benac; clay; composition; fig; flysch; landslide; minerals; samples; shear
• Mineralogy, surface properties and electrokinetic behaviour of kaolin clays from the naturally occurring pegmatite deposits by Ivanić, Maja; Vdović, Neda; Barreto, Sandra de; Bermanec, Vladimir; Sondi, Ivan (2015) - Sample Location Major component Minor component S1 Mamoes, Equador kaolinite muscovite, quartz S2 Jacu, Brazil kaolinite muscovite, quartz S3 Almas, Parelhas (2003) kaolinite muscovite, quartz, feldspars S4 Sierra Leone kaolinite muscovite, quartz, feldspars, smectites S5 Almas, Parelhas (2004) kaolinite muscovite, quartz, feldspars, smectites properties of clay mineral surfaces. The appear­ ance of these morphological features was confirmed by the FE-SEM images displayed in Figure 3A-D. These are charac­ terized by stacked pseudo-hexagonal platelets with diameters Geologia croatica 68/2Geologia Croatica 142 The CEC and SSA of kaolin clay samples are shown in Figure 4. Keywords: cec; clay; doi; kaolin; kaolinite; minerals; presence; properties; samples; sondi; ssa; surface
• Distribution of chemical elements in soil samples from the Pelagonia region, Republic of Macedonia by Puteska, Ana; Dimovska, Bojana; Šajn, Robert; Stafilov, Trajče (2015) -  Distribution of chemical elements in soil samples from the Pelagonia region, Republic of Macedonia  Ana Puteska1, Bojana Dimovska1, Robert Šajn2* and Trajče Stafilov1 1 Institute of Chemistry, Faculty of Natural Sciences and Mathematics, Ss Cyril and Methodius University in Skopje, POB 162, 1000 Skopje, Republic of Macedonia 2 Geological Survey of Slovenia, Ljubljana, Slovenia; (Robert.Sajn@geo-zs.si) doi: 10.4154/gc.2015.20 ABSTRACT This study represents the first systematic investigation of the spatial distribution of different chemical elements in the soil cover of the Pelagonia region, Republic of Macedonia. Distribution of chemical elements in soil samples from the Pelagonia region, Republic of Macedonia Geologia Croatica 263 tion in Macedonia and 30% of the wheat production. Keywords: analysis; distribution; elements; factor; macedonia; pelagonia; region; republic; samples; soil; subsoil; topsoil
• Properties of fly ash and slag from power plants by Šešlija, Miloš; Rosić, Aleksandra; Radović, Nebojša; Vasić, Millinko; Đogo, Mitar; Jotić, Milovan (2016) - In June, three samples of fly ash were selected, with a total of 36 samples of fly ash and four slag samples (Table 1). (in Serbian with English abstract) KIM, B., PREZZI, M. & SALGADO, R. (2005): Geotechnical Properties of Fly and Bottom Ash Mixtures for Use in Highway Embankments.– Journal of Geotechni- cal and Geoenvironmental Engineering, 131/7, 914–924. MILETIĆ, S. & ILIĆ M. (2007): Korišćenje elektrofilterskog pepela u građenju i građe- vinskim materijalima.– Association of Civil Engineers and Technicians of Serbia, Belgrade. SRPS B.H8.359 (1973): Methods of analysis of coal and coke – Determination of chem- ical composition of fuel ash – General requirements. SRPS B.H8.360 (1973): Methods of analysis of coal and coke – Determination of silica (SiO2) in ash from solid fuels. Keywords: ash; basin; chemical; coal; composition; fly; mineral; properties; samples; slag
• Croatian diatomites and their possible application as a natural insecticide by Galović, Ines; Halamić, Josip; Grizelj, Anita; Rozman, Vlatka; Liška, Anita; Korunić, Zlatko; Lucić, Pavo; Baličević, Renata (2017) - Quantitative mineral composition of samples (in wt. %) obtained by XRD analysis using RockJock® computer program (EBERL, 2003). The content of arsenic (As) is significantly lower in all ana- lysed samples compared to sample Celatom® MN 51 (Tab. 4). Keywords: celatom; content; coscinodiscus; croatian; diatomites; efficacy; ehrenberg; galović; grunow; korunić; ma­4; medvednica; miocene; opal; samples; sarmatian; silica; standard; tab; var
• Pore characterization, acoustic and permeability measurements on core plug triplets, from the Miocene Tótkomlós (Calcareous Marl) Formation of the Pannonian-basin, Hungary by Koroncz, Péter János; Péter, Ács; Lemberkovics, Viktor; Fedor, Ferenc (2017) - – Canadian Society of Exploration geophysicists re­ corder, 36/10, 38–43. MarTÍNEz, J.M., SCHMITT, D.r. & koFMaN, r. (2012): anisotropy measurements in a multi-faced core sample by using pulse transmission method, geoConvention, Calgary, alberta. oSTaDHaSSaN, M., zENg, z., JabbarI, H. (2012): anisotropy analysis in Shale using advanced Sonic Data – Extended abstract, bakken Case Study, aaPg an­ nual Convention and Exhibition, uSa. THoMMES, M., kaNEko, k., NEIMark, a.v., oLIvIEr, J.P., roDrIguEz-rEI­ NoSo, F., rouQuEroL, J. & SINg, k.S.W. (2015): Physisorption of gases, with special reference to the evaluation of surface area and pore size distribution (IuPaC Technical report). 5. RESULTS AND INTERPRETATION Figure 6. shows acoustic velocity measurements as a function of confining pressure. Keywords: anisotropy; c c; calcareous; case; core; figure; marl; measurements; pressure; samples; stress; wave
• Significance of the Badenian petroleum source rocks from the Krndija Mt. (Pannonian Basin, Croatia) by Zečević, Marko; Velić, Josipa; Sremac, Jasenka; Troskot-Čorbić, Tamara; Garašić, Vesnica (2010) - 2. MATERIALS, DATA AND METHODS OF RESEARCH Detailed analysis in the fi eld, and scans of geological col- umns, has yielded rock samples selected for mineralogical, petrographic, geochemical and organogeochemical analyses. Zecevic.indd 225 � AB STRA CT Discovery of petroleum source rocks at surface exposures of the Badenian deposits on the northern slopes of Krn dija Mt. is the fi rst record of petroleum source rocks at outcrop in the Croatian part of the Pannonnian basin. Keywords: badenian; basin; bukova; column; content; croatia; data; fig; glava; krndija; matter; pannonian; petroleum; research; rocks; samples; sediments; signifi; source
• Hyperspectroscopic and microtopographic analyses of salt crust forms on arid, silty clay loam desert soils by Howari, Fares M.; Al Aydaroos, Fatima; Nazzal, Yousef; Iqbal, Jibran; Bou Orm, Nadine (2019) - WANG, X., ZHANG, F., DING, J., KUNG, H.T., LATIF, A. & JOHNSON, V.C. (2018): Estimation of soil salt content (SSC) in the Ebinur Lake Wetland National Nature Reserve (ELWNNR), Northwest China, based on a Bootstrap-BP neural network model and optimal spectral indices.– Samples of salt affected soils and associated salt crusts that represented a range of soil salini- ties, slope, and moisture contents were gathered from the banks of the Rio Grande. Keywords: crusts; gypsum; halite; howari; minerals; moisture; reflectance; reflectivity; remote; salt; samples; sensing; slope; soil; spectral
• Distribution of major and trace elements in the Kovin lignite (Serbia) by Životić, Dragana; Cvetković, Olga; Vulić, Predrag; Gržetić, Ivan; Simić, Vladimir; Ilijević, Konstantin; Dojčinović, Biljana; Erić, Suzana; Radić, Bogdan; Stojadinović, Sanja; Trifunović, Snežana (2019) - Coal seam II The geochemical composition of coal seam II shows some diffe­ rences between fields A and B. Organic matter of the lignites from both coalfields was derived from herbs and shrubs with variable amounts of woody vegetation (MITROVIĆ et al., 2016). The content of As, Cr, Ni, Pb, V and Zn in seam II coal is several times higher in comparison with the Clarke values for brown coal (KETRIS & YUDOVICH, 2009). Keywords: ash; coal; coal geology; coal seam; content; doi; elements; et al; field; fig; iii; journal; kovin; kovin lignite; lignite; minerals; samples; seam; seam ii; serbia; table; trace
• Holocene foraminiferal and geochemical records in the coastal karst dolines of Cres Island, Croatia by Brunović, Dea; Miko, Slobodan; Ilijanić, Nikolina; Peh, Zoran; Hasan, Ozren; Kolar, Tena; Šparica Miko, Martina; Razum, Ivan (2019) - The geochemical and mineralogical signature is typical for terra rossa soils developed in carbonate terrains (DURN et al., 1999; MIKO et al., 2001). Analysed sam- ples from the lowermost part of the core exhibit similarity in geo- chemical and mineralogical composition to the basal part of the LK-2 core (Fig. 10) and indicate terrestrial soil (DURN et al., 1999; MIKO et al., 2001). Keywords: adriatic; analysis; arcij; assemblages; coast; concentrations; conditions; core; cres; croatia; data; debenay; doi; environments; et al; fig; foraminifera; holocene; island; karst; level; lk-2; lk-3; lk-6; marine; marinska; pond; samples; sea; sediment; species; unit; water
• Macroscopic, optical and diffraction assessment of encrustations and SEM analyses of phototrophic microbial mats from wellheads and select zones of emergence of mineral water in Serbia by Šaraba, Vladimir; Popović, Slađana; Obradović, Vesna; Štrbački, Jana; Gajić, Violeta; Vulić, Predrag; Subakov Simić, Gordana; Krunić, Olivera (2019) - Sampling of mineral waters Samples of mineral water for physical and chemical analyses were collected in plastic bottles. WOYESSA (2012) reports data on carbonate encrustation from mineral waters with pH levels lower than 8.3, which is the case in the present study (pH: BB-1– 6.9; LB-4 – 7.5; LB-5 – 6.6; VG-2 – 7.9; VG-3 – 8.0) (Tab. 2), and APPELO & POSTMA (2004) state that carbonate encrustations are dominant at pH˂8.3. Conductivity, a property of mineral water determined in situ, which depends on the concentration of dissolved salts, measured higher values in Lukovska Banja and Vranjska Banja (wells: LB-4 – 1513 μS/cm; LB-5 – 1588 μS/cm; VG-2 – 1584 μS/cm; VG-3 - 1707 μS/cm). Keywords: analyses; aragonite; banja; bb-1; bogatić; calcite; calcium; carbonate; doi; encrustations; fig; lb-4; lb-5; lukovska; lukovska banja; mineral; mineral water; precipitation; samples; serbia; vg-2; vg-3; vranjska; vranjska banja; water; wells
• Northern Velebit (Croatia) karst hydrological system: results of a preliminary 2H and 18O stable isotope study by Paar, Dalibor; Mance, Diana; Stroj, Andrej; Pavić, Mirja (2019) - The average d-excess value of cave collected samples is (14.89 + 1.26) ‰. Approximately constant d-excess values of cave water samples indicate the absence of significant evaporation before infiltration, i.e. fast infiltration of precipitation to the epikarst storage. Basic information about spring water samples. Keywords: caves; doi; fig; groundwater; isotope; karst; precipitation; samples; sampling; system; values; vcs; velebit; water
• Geochronology, geochemistry, and tectonic significance of the Shirenshan gneiss in the southern margin of the North China Block by Wang, Jingya; Ren, Shenglian; Dong, Shuwen; Longming, Li; Jiang, Dazhi; Shi, Yonghong; Li, Jiahao; Song, Chuanzhong; Han, Xu; Li, Zhenqiang; Ouyang, Jue (2019) - The partial melt was then intruded into the Taihua group in a “wedge-shape” and deformed together with the Luoluan fault zone to form the granitic gneiss – Shirenshan gneiss. The Shirenshan block consists of granite, Shirenshan gneiss and the Taihua group migmatite from north to south, respec- tively. Keywords: age; block; china; elements; et al; gneiss; granite; group; margin; north; samples; shirenshan; shirenshan gneiss; taihua; type; zircon
• Geochemistry and U-Pb ages of the diabases from the Luoji area, western Yunnan, China: implications for the timing of initial rifting of the Ganzi-Litang Ocean by Wang, Chan; Liu, Hao; Feng, Hanbin; Deng, Jianghong; Liu, Xianfan; Zhao, Fufeng (2019) - et al., 2015; KHOSHNOODI et al., 2017; ZHOU et al., 2018). So a large number of diabase samples were sought in this study to find out the CRB samples. Keywords: diabases; diagram; doi; et al; fig; ganzi; litang; luoji; mantle; ocean; samples; vs.; wang; wt.%; zircon
• Comprehensive characterization of bentonites from Croatia and neighboring countries by Gverić, Zvonka; Hanžel, Darko; Kampić, Štefica; Pleša, Andrej; Tibljaš, Darko (2020) - This diagram shows that most samples originate from acidic to neutral volcan­ oclastic material, with sample BD standing out as andesitic in composition. For ex­ ample, the calculated layer charge for BU and, to lesser extent, for BD samples is too high for smectites, yet the Mg­test did not show the presence of vermiculite in those samples. Keywords: bentonite; cations; charge; chemical; clay; content; croatia; doi; k 0; layer; mineral; miocene; peak; samples; smectites; table; ši1
• Lithostratigraphy and Sedimentological Characteristics of the Calciturbidites of the Babadağ Formation-Tavas Nappe (SW Turkey) by Kore, Basiru Mohammed ; Gül, Murat; Küçükuysal , Ceren ; Sarı, Bilal (2021) - The Beydağları Autochthone includes Late Triassic­Creta­ ceous platform carbonates and the Lutetian­Miocene sediments (Fig. 3; ERSOY, 1990; ŞENEL et al., 1989, 1994, 1998; SARI & ÖZER, 2001; 2002; SARI et al., 2004; SARI, 2006; 2017; ŞENEL, 2004, 2007; SOYCAN et al., 2015). The Lycian Nappes (including deep­water sediments of the Tavas Nappe), have since become a subject of widespread interest for numerous researchers over the last four decades, focusing on the fossil content and local lithological chara­ cteristic of the units (YILMAZ, 1981; ERAKMAN et al., 1982; ŞENGÖR et al., 1984; OKAY, 1989; ŞENEL et al., 1994; KO­ ZUR, 1998; COLLINS & ROBERTSON, 1998, 1999; ÖZCAN et al., 2012; GÜL et al., 2013; GÜL, 2015; SOYCAN et al., 2015; SARI, 2017). Keywords: babadağ; bedded; bozburun; calcilutite; calcite; calciturbidites; carbonate; chert; cretaceous; doi; et al; facies; fig; formation; gül; hill; lycian; nappe; robertson; samples; sea; section; sediment; slope; smf; tavas; turkey; western; yangı; şenel

• Healed injury in a nektobenthic trilobite: “Octopus-like” predatory style in Middle Ordovician? by Fatka, Oldrich; Budil, Petr; Mikuláš, Radek (2022) - Areiaspis BUDIL et al. (2007, p. 68) and MERGL et al. (2008, p. 277) clas­ sified rare specimens of this genus as deeper-water nektonic or benthic trilobites. al. (2018, 2021 and 2022) suppose that tri­ lobites could damage other trilobites. Keywords: basin; budil; czech; doi; et al; fatka; formation; geol; middle; ordovician; prague; republic; trilobites
• The calcareous nannofossil record of the uppermost Maastrichtian-lower Palaeocene in the Kırıkkale Basin, in the Central Anatolian Region (Turkey) by Kaya Ozer, Caner; Kilic, Yakup (2022) - YILDIZ et al. (2000) investigated the biostratigraphy and palaeoecology of the Lower Maastrichtian–Paleocene sedimentary units, using trace fossils, planktonic foraminifera and calcareous nannofossils. They also determined the δ18O and δ13C isotope values from planktonic foraminifera tests and compared these with the abun- dance distributions of calcareous nannofossils purported to be sensitive to temperature, finding that the sea-surface water tem- perature and salinity were lower in the Early Maastrichtian than the Palaeocene, increasing from the beginning of the Danian. AKORALER (2018) and GORMUS & AKORALER (2019) in- vestigated the benthic foraminiferal biostratigraphy and palaeo- ecology of the Late Cretaceous and Maastrichtian sedimentary deposits of the Kırıkkale and Kalecik regions. Keywords: base; basin; calcareous; cretaceous; cruciplacolithus; danian; doi; et al; f f; f r; f vr; fig; formation; kırıkkale; maastrichtian; nannofossil; r r; sample; section; species; vr ko; vr vr
• The New flora from the Permian of the Intrasudetic Basin, Poland by Šimunek, Zbynek; Ploch, Izabela (2022) - The Viséan consists of a few kms of fluvial and alluvial-fan deposits with in- tercalated marine to deltaic intervals (TÁSLER et al., 1979, Article history: Manuscript received January 03, 2021 Revised manuscript accepted March 24, 2022 Available online June 23, 2022 Keywords: Permian, Intrasudetic Basin, Poland, Flora, Alloiopteris G eo lo gi a C ro at ic a Geologia Croatica 75/2200 BOSSOWSKI, 1995). Developing a clear stratigraphy for the Intrasudetic Basin took a long time (KREJČÍ, BEYRICH, JOKÉLY, O. FEISTMANTEL, STUR and WEISS), and most of these works concerned the Carboniferous “coal-bearing” de- posits. Keywords: alloiopteris; barthel; basin; czech; fig; figs; flora; intrasudetic; janików; lobatopteris; locality; permian; species; specimens
• Middle Miocene (Late Badenian) microvertebrates from Hidas, SW Hungary by Hír, János; Venczel, Márton; Sebe, Krisztina (2024) - Cro- codylian�finds�reported�earlier�from�the�Hidas�Formation�indicate�a�subtropical�climate,�just�before� the�end�of�the�Miocene�warm�period�in�Central�Europe.�Among�the�rodents,�glirids�and�flying�squir- rels as well as Democricetodon and Megacricetodon indicate the presence of humid arboreal veg- etation�around�the�site.�The�rodent�taxa�are�well�known�from�the�Middle�Miocene�faunas�of�north- ern�Hungary,�western�Romania�and�from�the�Upper�Freshwater�Molasse�of�southern�Germany� and Switzerland. Consequently, although the coeval palaeogeography of the region has been described�as�an�archipelago�in�the�Central�Paratethys,�with�the�Mecsek�Mts.�being�one�of�the�is- lands, the area must have had ecological connections towards the northern and eastern parts of the Pannonian Basin, and the marine areas within the archipelago did not form a barrier against the�distribution�of�microvertebrates.�The�corridor�could�have�been�located�towards�the�NE�from�the� Mecsek�Mts.,�across�the�elevated�basement�blocks�of�central�Hungary. Keywords: anterior; base; basin; democricetodon; der; doi; fig; hidas; hidas mmp; hungary; hír; labial; lingual; margin; material; middle; miocene; mmp; posterior; ridges; specimens; surface
• The Alps as the main source of sand for the Late Miocene Lake Pannon (Pannonian Basin, Croatia) by Matošević, Mario; Garzanti, Eduardo; Šuica, Sanja; Bersani, Danilo; Marković, Frane; Razum, Ivan; Grizelj, Anita; Petrinjak, Krešimir; Kovačić, Marijan; Pavelić, Davor (2024) - The model is based on insights gleaned from previous studies (e.g., MAGYAR et al., 2013; SZTANÓ et al., 2013; PAVELIĆ & KOVAČIĆ, 2018; SEBE et al., 2020; MATOŠEVIĆ et al., 2023; ŠPELIĆ et al., 2023) and the findings of this research. This knowledge is crucial for evaluating their potential as reservoir rocks, not only for traditional oil and gas exploration but also for emerging technologies such as carbon capture, utilization, storage, and geothermal energy initiatives (e.g., SNEIDER, 1990; HORVÁTH et al., 2015; MACENIĆ et al., 2020; ALCALDE et al., 2019; TUSCHL et al., 2022). Keywords: alps; basin; croatian; data; depression; doi; drava; et al; fig; geology; kovačić; lake; miocene; north; pannonian; pavelić; provenance; rocks; sandstones; sava; source
• Shale Volume, Seismic Attributes, and Proper Data Preparation: Critical Components for Modelling Subsurface Lithology Distribution by Kamenski, Ana; Kolenković Močilac, Iva; Cvetković, Marko (2025) - The presented methodology is limited to 3D seismic data due to the usage of a large number of attributes, some of which are not at all suited for calculation on 2D seismic data. Well data are often too sparse to enable meaningful inter- pretations using traditional methods, so the implementation of seismic data with advanced machine learning techniques is expected to yield better modelling results (SMIRNOFF et al., 2008; Keywords: attributes; basin; croatian; data; distribution; et al; input; kovačić; lithology; model; networks; pannonian; pavelić; shale; study; subsurface; values; volume
• Plio–Quaternary Geometry and Kinematics of Ptolemais Basin (Northern Greece): Implications for the Intra-Plate Tectonics in Western Macedonia by Diamantopoulos, Anastasios (2010) - A significant difference in deforma- tion style between the Vegoritis–Ptolemais and Ptol- emais–Kozani sub-basins is indicated by their different strike and internal morphology, and by the greater depth and width of the Vegoritis–Ptolemais sub-basin. Given this evi- dence, the following must be considered in a new inter- pretation of the structural evolution of the Ptolemais basin: a) a westward tilting of the sedimentary fill in the Ptole- mais–Kozani sub-basin and a west–northwestward tilting of the sedimentary fill in the Vegoritis–Ptole- mais sub-basin; b) a rhomb-like morphology of the Ptolemais–Kozani sub-basin (DIAMANTOPOULOS & DIMITRAKO- POULOS, 2004a); c) the left-lateral strike-slip fault in the western margin- al domain (DIAMANTOPOULOS, 2004); d) the co-existence of reverse and normal faults in all mines of the PPC; e) anticline structures with a NE–SW axis trend in the internal parts of the basin; f) the kinematics of the deformation of Pliocene lignites in the boundary between the Ptolemais–Kozani and Vegoritis–Ptolemais sub-basins (DIAMANTOPOU- LOS & DIMITRAKOPOULOS, 2004b); g) the deformation partitioning between the marginal zones of the basin (DIAMANTOPOULOS, 2004); h) the thickness variation of the Pliocene lignites and of the Plio–Quaternary sediments; i) the different stratigraphy and sub-surface morphol- ogy between the Ptolemais–Kozani and Vegoritis– Ptolemais sub-basins, making the stratigraphic cor- relations difficult (DIAMANTOPOULOS & DIMI- TRAKOPOULOS, 2004a), and j) the Quaternary ductile–brittle deformation of the basement-units in eastern Askion and the eastern Vernon mountains (DIAMANTOPOULOS, 2005). Keywords: basin; deformation; diamantopoulos; fig; greece; macedonia; plio; ptolemais; ptolemais basin; sub
• Mixed Clastic–Carbonate Cycles and Sequences: Quaternary of Egypt and Carboniferous of England by Tucker, Maurice E. (2010) - Lower mudrock – upper carbonate cycles In metre-scale (4th/5th order) carbonate cycles (para- sequences) with lower mudrock beds, the clays are usually deeper-water marine or lagoonal facies, derived from reworking of muddy coastal plains and supplied by rivers. Wide expanses of carbonate sand, mostly of calcareous algal origin, occur on the shelf off NE Brazil, where quartz- rich sands were deposited at times of glacially-lowered sea-level (TESTA & BOSENCE, 1998). Keywords: basin; carbonate; carboniferous; clastic; coast; cycles; deposition; fig; highstand; level; limestone; plate; platform; red; reef; sea; sequences
• Clastic Sediment Partitioning in a Cretaceous Delta System, Western Canada: Responses to Tectonic and Sea-Level Controls by Plint, A. Guy (2010) - The incision of valley systems is attributed in part to periods of eustatic fall. Analysis of palaeosols mantling interfluve surfaces between valley systems. Keywords: accommodation; allomembers; basin; canada; cretaceous; delta; dunvegan; facies; fig; formation; interfluve; marine; mccarthy; palaeosols; plain; plint; sediment; subsidence; surfaces; systems; valley; western
• Tertiary Subsurface Facies, Source Rocks and Hydrocarbon Reservoirs in the SW Part of the Pannonian Basin (Northern Croatia and South-Western Hungary) by Saftić, Bruno; Velić, Josipa; Sztano, Orsolya; Juhasz, Györgyi; Ivković, Željko (2010) - BÉRCZI et al., 1988; SZENTGYÖRGYI & JUHÁSZ, 1988; JUHÁSZ, 1991, 1994; HORVÁTH & TARI, 1999; PRELOGOVIĆ et al., 1998; LUČIĆ et al., 2001; VELIĆ et al., 2002). This supplied huge amounts of sediment via large fluvial to deltaic systems into Lake Pannon (BÉRCZI et al., 1988; SZENT- GYÖRGYI & JUHÁSZ, 1988; JUHÁSZ, 1991, 1994), resulting in the accumulation of post-rift sedimentary successions several thousand metres thick. Keywords: badenian; basement; basin; croatia; depression; drava; et al; fig; horváth; hungary; juhász; lake; miocene; neogene; pannonian; rocks; sandstones; sava; sediments; source; velić
• Facies and Facies Architecture of the Ivanić Grad Formation (Upper Pannonian) - Sava Depression, NW Croatia by Vrbanac, Boris (2010) - Thick bedded to massive sandstone facies (F2) This facies is represented by thick-bedded to massive homogenous sandstones with a few siltite and marl intercalations which can be compared to massive sand- stone facies (WALKER, 1978). According to the sedimentological properties of the cored deposits (lithology, bedding, texture, relation between lithological members) four facies were identi- fied: massive marl facies (F1), thick bedded to massive sandstone facies (F2), thin bedded sandstone facies (F3), and laminated sandstone, siltite and marl facies (F4) 2.2.1. Keywords: associations; basin; beds; channel; depression; facies; facies association; fig; formation; grad; ivaniê; marl; marl facies; oil; pannonian; parts; sandstone; sandstone facies; sediments; turbidite
• The Pannonian Palaeoecology and Biostratigraphy of Molluscs from Kostanjek - Medvednica Mt., Croatia by Vrsaljko, Davor (2010) - Many ostracod forms supply and test the stratigraphic val- ue of molluscs and support zonality of Pannonian layers. Lower Pannonian marls and clays of facies AB con- tain ostracod samples, which represent an overture for the later explosion and divergence of species (HAJEK- TADESSE, pers. Keywords: basin; community; fig; fossil; layers; marls; molluscs; pannonian; sarmatian; species
• Calcareous algae from Upper Albian - Cenomanian strata of the Potiguar basin (NE Brazil) by Granier, Bruno; Dias-Brito, Dimas; Bucur, Ioan I. (2008) - 1: Arizona and Texas, JOHNSON, 1954, 1965, 1968; KONISHI & EPIS, 1962; 2: Mexico, BARATTO- LO, 1983, 1990; 3: Guatemala, JOHNSON & KONISHI, 1960; JOHNSON & KASKA, 1965; 4: Venezuela, JOHNSON, 1965; 5–6: Brazil, 5: Potiguar, SRIVASTAVA, 1982a, 1982b, 1984, 6: Sergipe, BERTHOU & BENGSTON, 1988; GRANIER et al., 1991a, 1991b; 7: Nigeria, POIGNANT & LOBITZER, 1982; 8: Gabon, ROUSSELOT, 1995; 9: Congo, MASSE, 1995; 10: Angola, ROMANES, 1916. Tribe Salpingoporelleae BASSOULLET et al., 1979 Sub-Tribe Salpingoporellinae BASSOULLET et al., 1979 Genus Holosporella PIA, 1930 Holosporella nkossaensis P. MASSE, 1995 (Pl. 2, Fig. Keywords: algae; atlantic; basin; calcareous; fig; genus; geologia; johnson; neomeris; potiguar; south
• Organic Geochemistry in the Rationalization of Oil and Gas Exploration and Production by Barić, Gertrud (2010) - Source rocks are pre­ dominantly marly limestones and limy marls of Lower to Middle Miocene age, while bacteria-degraded algal matter and terrigenous lip ids are the precursors of petroleum t • Recent investigation established that thick, compact dark-gray (0 black carbonaceous fossiliferous mud - stones, clayey mudstones and si ltstones of Lower M iocene and Mesozoic age at depths exceeding 3,000 m in the Mura depression and in the western part of the Drava depression represent source rocks in these areas (Figs. 2 and 3). Research included the identifica­ tion of source rocks, genelic characteri za tion of hydro­ carbons within accumul ati ons, detennina tion of alter­ ation and destruction of hydrocarbons within reservoirs and ex planation of the mechanisms for the appearance o f high concentrations of chem ica ll y inorganic con- 192 KAAlOVAC KAAPINA ZAGREB @ CA)(OV~C VAAiIZOlN % SISAK - '<9l..~ KO~IVN1tA ~~, VII'!OVITICA ® POtEGA ® LEGEND _ OIlFIELD .,. Keywords: baric; basin; depression; exploration; fig; gas; geochemical; hydrocarbons; oil; reservoir; rocks; source
• How a Better Knowledge of the Basins Can Reduce the Risk of Exploration: Input of Basin Modelling by Mascle, Alan; Durand, Bernard (2010) - The benefit or such modclling work is three fold: a) to unite thc work or a multidisciplinary team and to make an atlcmpt to quantify geological data; The selec tion of the mode lli ng lools will also be depen­ dent on the availability of quality data. Keywords: basin; data; modelling
• gc-470 by None (None) - Within thicker megabeds, Unit 3 shows a transitional contact with the underlying Unit 2. No mega bed has been identified in the Alpago flysch; only one 7 m thick big bed is described by GNACCOLINI (1968). Keywords: basin; carbonate; del; detritus; eocene; fig; flysch; flysch del; friuli; grivo; julian; margin; megabeds; paleocene; platform; section; sequence; siliciclastic; southern; thick; thickness; tunis; turbidites; unit; venturini
• Composition and provenance of Neogene sedimentary rocks of Dilj gora Mt. (south Pannonian Basin, Croatia) by Kovačić, Marijan; Horvat, Marija; Pikija, Mato; Slovenec, Damir (2011) - The main goal of this study is to determine the compo- sition of clastic sedimentary rocks and reconstruct the origin of clastic material supplying the sediments of Dilj gora Mt. during the Neogene by integrating sedimentological and pet- rographic data. At that time Dilj gora Mt. area belonged to the southern part of Central Paratethys. Keywords: basin; clastic; composition; detritus; dilj; fig; geol; gora; material; miocene; pannonian; rocks; sediments; south; unit
• Reservoir Geology, Hydrocarbon Reserves and Production in the Croatian part of the Pannonian Basin System by Velić, Josipa; Malvić, Tomislav; Cvetković, Marko; Vrbanac, Boris (2012) - Other parameters listed for gas fi elds are charac- terised by similar trends observed for oil fi elds. For oil fi elds, group 1 reservoirs are sandstones of Pan- nonian and Pontian age, except for the Beničanci Field, where the reservoir is a Badenian breccia. Keywords: basin; croatian; data; elds; fi elds; gas; oil; pannonian; production; reserves; reservoirs; velić
• Middle and Late Miocene palynological biozonation of the south-western part of Central Paratethys (Croatia) by Bakrač, Koraljka; Koch, Georg; Sremac, Jasenka (2012) - The Karpatian/Badenian boundary is characterized by a signifi cant sea level fall (HAQ et al., 1988; HARDENBOL et al., 1998), expressed as a hiatus (“Styrian unconformity”), traceable throughout Central Paratethys (RÖGL et al., 2002, HARZHAUSER & PILLER, 2007). The transition from the Badenian to Sarmatian deposits is observed in Žumberak (VRSALJKO et al., 2005), Hrvatsko zagorje (Zaj-I; Fig. 1b) and Slavonija (Nac-I; Fig. 1c) (PAVELIĆ et al., 2003; VASILIEV et al., 2007). Keywords: agellate; badenian; basin; bentorii; central; croatica; dinofl; early; environments; et al; fig; late; mediterranean; middle; miocene; nac; pannonian; paratethys; sarmatian; sea; spiniferites; szentai; sütő; view; zone
• A reappraisal of the Carboniferous macrofloras of the Zonguldak – Amasra Coal Basin, north-western Turkey by Cleal, Chistopher J.; van Waveren, Isabel M. (2012) - X X X Alethopteris ambigua LESQUEREUX X X X X Alethopteris pseudograndinioides ZODROW & CLEAL X X ? 1 2 3 4 5 6 7 8 Sublepidodendron robertii (NATHORST) CHALONER X X X X X X X Eleutherophyllum mirabile (STERNBERG) STUR X X X Sphenophyllum tenerrimum ETTINGSHAUSEN X X X X X Pecopteris aspera BRONGNIART ? Keywords: age; amasra; basin; brongniart; carboniferous; cleal; coal; croatica; et al; formation; jongmans; kerey; late; macrofloras; plant; species; sternberg x; upper; wagner; zeiller; zeiller x; zone; zonguldak
• Comparison between the Middle Miocene and the Upper Miocene source rock formations in the Sava Depression (Pannonian Basin, Croatia) by Troskot-Čorbić, Tamara; Velić, Josipa; Malvić, Tomislav (2009) - Source rock intervals lay at depths from 1200 to 3362 m. The Total Organic Carbon (TOC) of analyzed samples varies from 0.39 to 4.94%, while their total ge nerative hydrocarbon potential is from 2.40 to 37.40 mg HC/g rock. Source rock Based on the results of organic geochemical analyses and organic petrography, source rock intervals were singled out in the drilled columns of 25 exploration wells in the Sava Depression area. Keywords: basin; depression; facies; fig; intervals; miocene; organic; pannonian; rock; sava; source; source rock
• Aspects of Romanian Palaeozoic Palaeobotany and Palynology. Part III. The Late Carboniferous flora of Baia Nouă, Sirinia Basin by Popa, Mihai Emilian; Cleal, Christopher J. (2012) - Croatica 332 Bituminous coals were first discovered here in 1840 and have been extracted since 1874 (RăILeaNU et al., 1963); mining activities in Baia Nouă ended in 2006 for safety and financial reasons. 9 Material: Casts of this fossil-species are abundant in the newly collected samples from Baia Nouă, such as frag- ment 1 of sample P51/C5/1 (Pl. 2, Fig. 1) in the M.E. Popa Collection (University of Bucharest). Keywords: baia; basin; biţoianu; bucharest; carboniferous; cleal; collection; croatica; fig; neuralethopteris; nouă; popa; sirinia; university; westphalian
• Pennsylvanian floras from Italy: an overview of the main sites and historical collections by Ronchi, Ausonio; Kustatscher, Evelyn; Pittau, Paola; Santi, Giuseppe (2012) - 17 shows a biostratigraphic and lithostratigraphic subdivision of the Pennsylvanian­Autunian succession, on the basis of different fossil floras found at various localities in the Valle del Guappero (from TRE­ VISAN, 1955 and RAU & TONGIORGI, 1974 in LANDI DEGLI INNOCENTI et al., 2008; mod.). TREVISAN (1955) indicated the index fossils for each fossil locality (from LANDI DEGLI INNOCENTI et al., 2008, mod.). Keywords: age; alps; basin; carboniferous; croatica; del; der; et al; fig; figure; floras; formation; fritz; geologia; italy; krainer; late; pennsylvanian; permian; pittau; plant; ronchi; sardinia; soc; southern; venturini
• Discriminant Function Analysis of Upper Miocene and Pliocene Sands from the Southwestern Part of the Pannonian Basin System, Croatia by Kovačić, Marijan; Peh, Zoran; Grizelj, Anita (2009) - The HZb unit (Upper Pontian) is widespread in the whole studied area, overlying conformably the older, And unit, and passing conformably upward into the overlying Cer and Plu units (Fig. 3). The content of garnet is slightly higher with part of the samples in the And unit (Fig. 4C) while the remaining three groups (Cer, HZb and Plu units) remain indifferent in this relationship sticking to the middle position with the least mean values. Keywords: analysis; basin; cer; composition; croatica; discriminant; function; groups; hzb; kovačić; miocene; oza; pannonian; plu; sands; system; unit
• Petrology, geochemistry and tectono-magmatic affinity of gabbroic olistoliths from the ophiolite mélange in the NW Dinaric-Vardar ophiolite zone (Mts. Kalnik and Ivanščica, North Croatia) by Lugović, †Boško; Slovenec, Damir; Schuster, Ralf; Schwarz, Winfried H.; Horvat, Marija (2015) - This time interval represents a period of accumulation of lithostratigraphically diverse material in the intra-oceanic trench (SLOVENEC et al., 2011). It was suggested that the Mt. Medved- nica mafic-ultramafic crustal sequence represents remnants of a proto-arc–forearc system that was initiated in the ROD in Bathonian times (SLOVENEC et al., 2011). Keywords: arc; basin; croatica; crust; et al; fig; gabbroic; gabbros; geochemical; group; ivanščica; jurassic; kalnik; lugović; mantle; medvednica; mélange; oceanic; ophiolite; rocks; rod; slovenec; subduction; zone
• Structural controls on petroleum migration and entrapment within the faulted basement blocks of Szeghalom Dome (Pannonian Basin, SE Hungary) by Molnár, Lászlo; M. Tóth, Tivadar; Schubert, Félix (2015) - Previous studies (CAINE et al., 1996; EVANS et al., 1997; MOLNÁR et al., 2014) on the make-up of fault zones de- fined two main structural elements: 1) the weakly disaggre- gated, densely fractured “damage zone”, which is generally associated with higher conductivity and permeability rela- tive to the undeformed protolith; and 2) the intensively de- Structural controls on petroleum migration and entrapment within the faulted basement blocks of the Szeghalom Dome (Pannonian Basin, SE Hungary)  Molnár, László, M. Tóth, Tivadar and Schubert, Félix Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Egyetem u. 2., H-6722, Szeged, Hungary (molnar.laszlo@geo.u-szeged.hu) doi: 10.4154/gc.2015.19 Geologia CroaticaGeologia Croatica Geologia Croatica 68/3 247–259 11 Figs. The large-scale spatial interpretation of fault zones in hydrodynamic systems can be problematic, especially with a lack of borehole cores, packer measurements or sophisti- cated modeling because the main structural elements are of- ten below the limit of seismic resolution (BEN-ZION & SAMMIS, 2003). Keywords: basement; basin; data; et al; fault; fault zones; fig; fluid; migration; szd; tóth; wells; zones
• Contribution to the knowledge of Cordaites species from the Kladno-Rakovník Basin, Middle Pennsylvanian (Bolsovian), Czech Republic by Šimunek, Zbynek; Haldovský, Jan (2015) - The palaeoeco- logical significance of papillae on Cordaites cuticles is discussed and is probably an adaptation to living on a peat substrate. The cell corners Geologia Croatica 68/2Geologia Croatica 100 are strongly cutinised in the stomatiferous band and a strongly cutinised crypt is present above the guard cells in Cordaites kladnoensis abaxial cuticle. Keywords: adaxial; bands; bar; basin; cells; cordaites; cuticle; czech; scale; scale bar; species; stomatal; subsidiary; wartmannii; šimůnek
• Exploring the potential of deep targets in the South Adriatic Sea: insight from 2D basin modeling of Croatian offshore by Mazzuca, Nicoletta; Bruni, Alessandro; Joppen, Thorsten (2015) - Exploring the potential of deep targets in the South Adriatic Sea: insight from 2D basin modeling of the Croatian offshore Geologia Croatica 239 The stratigraphic column representing the study area and its petroleum system elements was recon- structed from the regional geological setting, the inter- pretation of Croatian wells implemented with Italian well information and the interpretation of new seismic data acquired by Spectrum (Fig. 3). Exploring the potential of deep targets in the South Adriatic Sea: insight from 2D basin modeling of the Croatian offshore Geologia Croatica 241 • Jurassic (Malm), Dolomite 50% and Ooid 50%; • Cretaceous, Limestone (ooid grainstone); • Eocene, Limestone (ooid grainstone). Keywords: adriatic; basin; cretaceous; croatian; fig; jurassic; model; petroleum; source; triassic
• Pannonian ostracods from the southwestern Transylvanian basin by Kovács, Erika; Magyar, Imre; Sztanó, Orsolya; Pipík, Radovan (2016) - vaSiliev et al., 2010). Of the large brackish lakes that repeatedly formed during the history of the Paratethys, the Late Miocene-Early Pliocene Lake Pannon was probably the longest-lived (MÜLLER et al., 1999; HARZ- HAUSER & MANDIC, 2008). Keywords: basin; candona; doi; et al; fauna; fig; filipescu; hemicytheria; krstić; lake; marl; miocene; ostracod; outcrop; pannonian; species; water
• History of the Belanovica (Serbia) Neogene lake basin inferred from petrological and geochemical data by Marić, Dragana; Srećković-Batoćanin, Danica; Vasić, Nebojša; Radisavljević, Marija; Đekić, Tatjana (2019) - Lake basins were presented either according to their age and depressions where they have been developed (AN- ĐEL KOVIĆ et al., 1991; OBRADOVIĆ & VASIĆ, 2007) or were classified geographically, such as basins in northern, central and eastern Serbia (KRSTIĆ et al., 2003; DOLIĆ, 1986). The alternation of lake sediments with those formed in marsh or alluvial systems, sometimes with coal and/or oil shales resulted in highly diverse facies. Keywords: basin; belanovica; calcite; clastites; clayey; doi; et al; lake; marlstone; neogene; ppm; rocks; sediments; serbia; siltstone; unit; va-1; va-2
• Foraminifera – based estimation of water depth in epicontinental seas: Badenian deposits from Glavnica Gornja (Medvednica Mt., Croatia), Central Paratethys by Pezelj, Đurđica; Drobnjak, Lucija (2019) - Glavnica Gornja section with sampling points (G), number of benthic foraminifera species, Diversity indices (Fisher α index, Shannon-Wiener index, Equi- tability, Dominance), oxic - disoxic indicators, epifauna/infauna ratio, BFOI, estimated depths of sedimentary basin after Hohenegger method and modified P/B ratio, and percentage of planktonic taxa. [Ear­ ly Badenian benthic foraminifera from Glavnica Gornja locality – in Croatian].– Keywords: badenian; basin; croatian; depth; doi; d´orbigny; et al; foraminifera; geol; hohenegger; middle; miocene; paratethys; section; species; water
• Revision of the genus Cordaites UNGER from the Permian of the Intrasudetic Basin (Broumov Formation, Olivětín Member, Czech Republic) by Šimunek, Zbynek (2019) - Since then, tens of Cordaites species have been described based on leaf morphology and venation. BAR­ THEL (1976) was aware of the problem of the correct determina­ tion of Cordaites species and came to the conclusion that it is not possible to distinguish three long­leaved Cordaites species – Keywords: affinis; basin; cordaites; cuticles; fig; grand’eury; leaf; leaves; species; specimens; veins; venation; šimůnek
• A methodology for assessing the pressures on transboundary groundwater quantity and quality – experiences from the Dinaric karst by Stevanović, Zoran; Marinović, Veljko (2020) - It should be noted that risk assessment methods are rather country­specific and range from using combinations of the afore-mentioned data sets to focus on interpreting water quality data. In the last few decades, sustainable water development and the de- mand for equitable sharing of water resources were included in numerous technical and legislative documents, articles and pro- jects dealing with transboundary groundwater (ECKSTEIN & ECKSTEIN, 2005; PURI & AURELI, 2005; PURI & STRUCK- MEIER, 2010). Keywords: aquifer; assessment; basin; data; groundwater; gwbs; hazard; karst; management; map; methodology; monitoring; pressure; quality; quantity; reserves; resources; risk; river; stevanović; vulnerability

• Uplifted Pleistocene marine sediments of the Central Adriatic Island of Brusnik by Babić, Ljubomir; Crnjaković, Marta; Asmerom, Yemane (2012) - Tectonic deformation in the area has continued until the present (ALJINOVIĆ et al., 1987; FAV- ALI et al., 1993; KUK et al., 2000; OLDOW et al., 2002; PRE LOGOVIĆ et al., 2003; HERAK et al., 2005; BENNETT et al., 2008; see also faults in Fig. 2 based on HERAK et al., 2005). Active tec- tonic boundaries and epicentres located close to Brusnik Is- land (ALJINOVIĆ et al., 1987; FAVALI et al., 1993; KUK et al., 2000; OLDOW et al., 2002; PRELOGOVIĆ et al., 2003; HERAK et al., 2005; BENNETT et al., 2008) may be relevant for tsunamogenic potential. Keywords: adriatic; brusnik; central; conglomerates; et al; fig; island; level; limestones; marine; pleistocene; rocks; sea; sediments
• Petrochronological study of chloritoid schist from Medvednica Mountain (Zagorje Mid-Transdanubian zone, Croatia) by Mišur, Ivan; Balen, Dražen; Klötzli, Urs; Belak, Mirko; Massonne, Hans-Joachim; Brlek, Mihovil; Brčić, Vlatko (2023) - The northern boundary of the ZMTZ is the Periadriatic transcurrent fault merging eastward into the Balaton line (FODOR et al., 1998; HAAS et al., 2000; TOMLJENOVIĆ et al., 2008; and reference therein). ŠIKIĆ et al., 1978; 1979; BASCH, 1983a,b; BABIĆ et al., 2002; JUDIK et al., 2004; LUGOVIĆ et al., 2006; TOMLJENOVIĆ et al., 2008; VAN GELDER et al., 2015). Keywords: age; analyses; chlorite; chloritoid; conditions; croatia; doi; et al; fig; medvednica; mica; mnz; monazite; quartz; rim; rocks; sample; schist; st-6; white; zone
• Petrography and geochemistry of granitoids and related rocks from the pre-Neogene basement of the Slavonia-Srijem Depression (Croatia) by Šuica, Sanja; Garašić, Vesnica; Woodland, Alan B. (2022) - Photomicrographs of: a) K-feldspar (Kfs) and quartz (Qtz) in equigranular alkali granite type 1 (B-1-5); b) clusters of albite (Ab), biotite (Bt) and hornblende (Hbl) with chlorite (Chl) and epidote (Ep) replacing albite in alkali granite type 1 (B-1-5); c) albite (Ab), sericitized K-feldspar (Kfs) and quartz (Qtz) in alkali granite type 2 (B-2-1); d) K-feldspar (Kfs), albite (Ab) and quartz (Qtz) in syenite (B-3-5), interstitial biotite (Bt); e) granite (B-6-2) with quartz (Qtz) and K-feldspar (Kfs) con- taining albite (Ab) inclusions; f ) rounded quartz (Qtz) phenocrysts, K-feldspar (Kfs) with albite (Ab) inclusions, sericite (Ser) in groundmass of rhyolite (B-6-2R); g) K- feldspar (Kfs) microcline (Mc), quartz (Qtz) and biotite (Bt) in gneiss (B-5-2); h) K-feldspar (Kfs) porphyroclast mantled by quartz (Qtz) and secondary chlorite (Chl) in gneiss (B-4-5). reports the results of petrography and whole-rock geochemistry for two types of alkali granite, granite, syenite, rhyolite and ortho- gneiss as well as the mineral chemistry for alkali granite type 1. Keywords: albite; alkali; b-1; biotite; croatia; doi; element; et al; feldspar; fig; granite; granite type; mineral; orthogneiss; pamić; quartz; rhyolite; rocks; syenite; types
• Dating and geochemistry of zircon and apatite from rhyolite at the UNESCO geosite Rupnica (Mt. Papuk, northern Croatia) and the relationship to the Sava Zone by Schneider, Petra; Balen, Dražen ; Opitz, Joachim; Massonne, Hans-Joachim (2022) - | www.geologia-croatica.hr Journal of the Croatian Geological Survey and the Croatian Geological Society 1. INTRODUCTION Mt. Papuk, situated at the southern edge of the Pannonian basin in northern Croatia (Fig. 1a), is characterized by a complex geo- logical evolution that comprises several orogenic events (JAMIČIĆ, 1983; BALEN et al., 2006, 2013; HORVÁTH et al., 2010). A-type granite of Mt. Požeška Gora The A-type granite of Mt. Požeška Gora (PAMIĆ, 1987; PAMIĆ et al., 1988/89; PAMIĆ & LANPHERE, 1991b) has been reinves- tigated in detail by BALEN et al. (2020), who confirmed a Late Cretaceous age (83.6±1.5 Ma) by U-Th-Pb dating on zircon. Keywords: apatite; balen; croatia; dating; doi; et al; fig; geochemistry; gora; granite; l. 0; mean; pamić; papuk; požeška; ratios; rhyolite; rocks; rupnica; type; volcanic; zircon; zone
• First occurrence of dumortierite in Croatia: its chemical composition and appearance as an igneous mineral in leucogranite-hosted pegmatite by Garašić, Vesnica; Lugović †, Boško; Krsnik, Mirjana; Bilić, Šime; Meyer, Hans-Peter; Schuster, Ralf; Vrkljan, Maja (2024) - This sequence is intruded by various types of gra- nitic rocks, such as two-mica granite, granodiorite, monzogran- ite and leucogranite (CRNKO & VRAGOVIĆ, 1990; PAMIĆ, 1990) as well as different types of gabbro (KIŠPATIĆ, 1887; TUĆAN, 1953; PAMIĆ, 1987; BALEN et al., 2003). This is in agreement with amphibole Ar-Ar cooling ages of 80-90 Ma determined for amphibolites (BALEN et al. 2001). Keywords: andalusite; biotite; chemical; composition; croatia; doi; dumortierite; et al; fig; gora; leucogranite; mineral; moslavačka; muscovite; pegmatite; pfu; rocks
• Middle Triassic basaltic pyroclastic rocks from the Mt. Medvednica ophiolitic mélange (NW Croatia): petrology, geochemistry and tectono-magmatic setting by Slovenec, Damir; Halamić, Josip; Šegvić, Branimir (2024) - However, the research presented here shows that, in Middle Triassic basaltic pyroclastic rocks from the Mt. Medvednica ophiolitic mélange (NW Croatia): petrology, geochemistry and tectono-magmatic setting Damir Slovenec1,*, Josip Halamić1 and Branimir Šegvić2 1 Croatian Geological Survey, Department of Geology, Sachsova 2, 10000 Zagreb, Croatia; (*corresponding author: damir.slovenec@hgi-cgs.hr) 2 Texas Tech University, Department of Geosciences, 1200 Memorial Circle, Lubbock TX 79409, U.S.A. doi: 10.4154/ Middle Triassic basaltic pyroclastic rocks from the Mt. Medvednica ophiolitic mélange (NW Croatia): petrology, geochemistry ... terized by porphyritic structure and almond-shaped texture (Figs. Keywords: alkali; basaltic; basalts; croatia; doi; et al; fig; medvednica; middle; mélange; ophiolitic; pyroclastic; rocks; slovenec; triassic
• Jabuka Shoal, a New Location with Igneous Rocks in the Adriatic Sea by Juračić, Mladen; Novosel, Anđelko; Tibljaš, Darko; Balen, Dražen (2010) - The major element content of Jabuka Shoal rocks is similar with those of the nearby Jabuka Islet magmatic rocks. Petrographic data reveal that the samples from Jabuka Shoal have similar structural, textural and compositional features compared to the ~2 km distant Jabuka Islet as described in detail in BALOGH et Keywords: adriatic; brusnik; islet; jabuka; jabuka shoal; rocks; sea; shoal
• Compositional Zoning in Amphibole from Amphibole Bearing Parageneses of West Psunj (Croatia): Evidence for Progressive Metamorphism? by Balen, Dražen; Bermanec, Vladimir; Marci, Vera (2010) - The change in P-T conditions recorded in the growth of amphibole grains (gcncral prograding patt crn) togcthcr with ch:mgcs in thc modal com­ positions in rclated paragcncscs could bc intcrprcted in a model of a subduction zone. Zonal growth of amphibole grains is a result of mul­ tiple periods of mineral growth. Keywords: amphibole; angle; assemblage; changes; epidote; facies; grains; green; growth; mineral; plagioclase; pressure; rocks; thc; type
• The Helicoidal Fault Systems of Vinodol (Croatia) and Their Genesis by Blašković, Ivan (2010) - U nKeywords: bora; carbonate; convergent; deformation; dip; echelon; fault; fig; geol; kao; orientation; phase; rasjeda; reverse; rocks; stress; strike; structures; systems; vinodol
• Pliocene Source Rocks, Miocene Reservoir Rocks and Origin of the Gas Accumulation of the Irma Field (Northern Adriatic, Croatia) Based on Wireline-Logging by Vulama, Ivica (2010) - ZAGREB 1997 Pliocene Source Rocks, Miocene Reservoir Rocks and Origin of the Gas Accumulation of the Irma Field (Northern Adriatic, Croatia) Based on Wireline-Logging Ivica VULAMA Key words: Pliocene source rocks, Miocene reservoir rocks, Messini an unconformity, Wirc line logging, Geochemical analysis, Discriminant function, Over­ pressure zone, Biogcnc gas, Middle Adria tic ridge, Croatia. 15 Kerogen Iype and maturity of Pliocene source rocks of tile Middle Adriatic ridge. Keywords: adriatic; analysis; bulk; density; fig; figs; gas; irma; line; logging; middle; miocene; pliocene; porosity; resistivity; ridge; rocks; sonic; source; source rocks; time; transit; zone
• Effectiveness of the Acidizing Treatment in Wells Based on the Petrographic Results of Thin-Section Acidizing Experiments by Raškaj, Nevenka; Gašljević-Miljovski, Edita; Hot-Grgić, Melika (2010) - Pene tratio n o f ac ids is onl y poss ib le a long the open or carbonate cemented fractures. Dependi ng on the m inera l composition, th in-sec ­ ti ons were ac id ized with hydrochlori c ac id and with a mixture o f hydrochloric and hydro Keywords: rocks
• First Rock Magnetic and Palaeomagnetic Analyses of the Pre-Cenozoic Rocks of the Velebit Mt. (Croatia): Prospects for Applications in Palaeogeographic and Geotectonic Studies by Lewandowski, Marek; Velić, Ivo; Sidorczuk, Magdalena; Vlahović, Igor; Velić, Josipa (2011) - Rock magnetic results Rock magnetic studies revealed the presence of both soft and hard magnetic phases in the studied rocks. 10H, I) show a similar NRM structure, recorded in rock samples collected at different sites. Keywords: components; croatia; demagnetization; fig; geologia; jurassic; magnetic; middle; márton; nrm; permian; results; rocks; velebit
• Source Rock generative potential and volumetric characteristics of Kurrachine Dolomite Formation, Hayan Block, central Syrian Palmyrides by Vulama, Ivica (2011) - A calculated volumetric characteristic of source rocks indicates their high hydrocar- bon generating capability. Keywords: Source rock, Triassic, Kurrachine Dolomite Formation, Amanus Shale Formation, Amanus Sand For- mation, Volumetric characteristics, Hydrocarbons generated, Petroleum System, Palmyrides, Syria Source rock generative potential and volumetric characteristics of the Kurrachine Dolomite Formation, Hayan Block, central Syrian Palmyrides � Ivica Vulama 1Exploration Department, INA Oil Company, A. V. Holjevca 10, 10 000 Zagreb, Croatia; (ivica.vulama@ina.hr) doi: 104154/gc.2011.22 Geologia Croatica 64/3 259–272 14 Figs. Keywords: block; characteristics; dolomite; formation; hydrocarbons; kurrachine; oil; reservoir; rocks; shale; source; source rocks; triassic
• Mafic enclaves in peraluminous Variscan granitoid in the Battonya Unit from Southeast Hungary by Buda, Gyorgy; Pál-Molnár, Elemér; Koller, Friedrich (2012) - Mafi c enclaves in peraluminous Variscan granitoid in the Battonya Unit from Southeast Hungary Geologia Croatica 245 Europe started in the Late Triassic–Early Cretaceous, as re- corded by crystalline rocks (BUDA et al., 2004/b) and sedi- mentary sequences (HAAS et al., 2004; CSONTOS et al., 2004; SCHMID et al., 2008). The possible isobaric cooling path of Battonya peraluminous granitoids is shown between the two arrows, (after CLARKE, et al.,2005). Keywords: battonya; biotite; fig; granite; granitoid; mica; muscovite; primary; rocks; unit; variscan
• Evidence of the spreading culmination in the Eastern Tethyan Repno oceanic domain, assessed by the petrology and geochemistry of N-MORB extrusive rocks from the Mt. Medvednica ophiolite mélange (NW Croatia) by Slovenec, Damir; Lugović, Boško (2012) - The ocean ridge affinity of the Poljanica rocks is also deduced from their high Ti/V ra- tio (32.9–42.6), that is typical for MORB rocks derived from a slightly depleted mantle reservoir (Fig. 5). The domain lacks ophiolite complexes and oceanic rocks are restricted to four Early Callovian to Late Valanginian ophiolite mélange sectors integrated in the Kalnik Unit. Keywords: basalts; et al; fig; geol; lugović; mantle; medvednica; morb; mélange; oceanic; ophiolite; rocks; slovenec; spreading
• Obituary Professor Boško Lugović, PhD by Aljinović, Dunja; Garašić, Vesnica (2013) - doi: 10.4154/GC.2012.32 ŠEGVIĆ, B., ŠEŠELJ, L., SLOVENEC, DA., LUGOVIĆ, B. & FER- REIRO MÄHLMANN, R. (2012): Composition, technology of manufacture, and circulation of Hellenistic pottery from the Eastern Aljinović and Garašić: Obituary Professor Boško LUGOVIĆ, PhD Geologia Croatica 247 Adriatic: a case study of three archaeological sites along the Dalma- tian coast, Croatia.– Geoarchaeology, 27, 63–87. Aljinović and Garašić: Obituary Professor Boško LUGOVIĆ, PhD Geologia Croatica 249 USTASZEWSKI, K., SCHMIDT, S.M., LUGOVIĆ, B., SCHUSTER, R., CARON, M., RETTENMUND, C., & KOUNOV, A. (2006): Does the Sava-Zone represent a remnant of the Vardar ocean and when did it close? Keywords: adriatic; boško; boško lugović; croatia; lugović; ophiolite; phd; professor; rocks; slovenec
• Bulk and clay mineral composition indicate origin of terra rossa soils in Western Herzegovina by Durn, Goran; Ćorić, Radica; Tadej, Neven; Barudžija, Uroš; Rubinić, Vedran; Husnjak, Stjepan (2014) - Namely, soils may contain “detrital”clays inheri- ted from the parent material (in this case soil clays represent the IR of carbonate rock) and they may contain clays formed by sequential weathering of unstable parent minerals of the IR (including clay mineral phases). Terra rossa B horizons have characteristic red colours, neutral to slightly acid pH, high base sat- uration with calcium as the predominant cation and high CIA (Chemical Index of Alteration). Keywords: carbonate; clay; composition; content; fraction; herzegovina; horizons; kaolinite; kočerin; mineral; residue; rocks; rossa; soil; terra; terra rossa; uzarići; čitluk
• Geochemical implications for the magma origin of granitic rocks from the Ditrău Alkaline Massif (Eastern Carpathians, Romania) by Pal-Molnar, Elemer; Batki, Aniko; Odri, Agnes; Kiss, Balazs; Almasi, Eniko (2015) - Keywords: A-type granite; geochemistry; mantle differentiates; amphibole geobarometry; Ditrău Alkaline Massif, Eastern Carpathians, Romania A wide variety of igneous rocks have been described in the DAM from ultramafic to mafic ones (Tarniţa Complex: peridotites, gabbros, diorites), felsic silica-saturated and oversaturated syenites and granites, as well as undersaturated alkaline rocks (nepheline syenites) (PáL-MOLNáR, 2000). In this paper we discuss new geochemical and petrolog- ical data on granites and draw conclusions on processes of magma evolution in order to provide further constraints on the formation of the Ditrǎu Alkaline Massif. Keywords: alkaline; amphibole; content; croatica; dam; ditrău; granites; massif; molnár; pál; rocks; type
• The Rudnik Mts. volcano-intrusive complex (central Serbia): An example of how magmatism controls metallogeny by Cvetković, Vladica; Šarić, Kristina; Pécskay, Zoltán; Gerdes, Axel (2016) - The Rudnik Mts. volcano-intrusive complex (central Serbia): An example of how magmatism controls metallogeny 97 different variation paths for dacite-andesite and quartzlatite rocks of the Rudnik Mts complex are given in Figures 7a, b. LE BAS, M.J., LEMAITRE, R.W., STRECKEISEN, A. & ZANETTIN, B. (1986): A chemical classification of volcanic rocks based on the total alkali- silica diagram.– Journal of Petrology, 27, 745–750. LOFGREN, G. (1971): Experimentally produced devitrification textures in natural rhyolitic glass.– Geological Society of America Bulletin, 82, 111–123. Keywords: complex; cvetković; dacite; et al; figure; magma; mineralization; mts; prelević; quartzlatite; rocks; rudnik; rudnik mts; serbia; volcanic; volcano
• Alkali Metasomatism and Th-REE Mineralization in the Choghart deposit, Bafq district, Central Iran by Khoshnoodi, Khalegh; Behzadi, Mehrdad; Gannadi-Maragheh, Mohammad; Yazdi, Mohammad (2017) - The negative Eu anomaly in Th mineralization zone, as well as the paragenetic occurrence of magnetite, pyrite and chalcopyrite with thorite suggest that Th-REE mineralization formed in relatively reduced condition. doi: 10.1007/978-3-642- 28394-9_7 POLLARD, PJ. (1983): Magmatic and post-magmatic processes in the formation of rocks associated with rare element deposits.– Keywords: apatite; bafq; choghart; deposit; district; elements; figure; iran; magnetite; metasomatism; mineralization; ore; ree; ree mineralization; rocks; thorite; type; zone
• The first record of ultramafic cumulates from the Mt. Kalnik ophiolite mélange in the SW part of the Zagorje-Mid-Transdanubian Zone (NW Croatia): mineralogy, petrology, geochemistry and tectono-magmatic affinity by Slovenec, Damir; Šegvić, Branimir (2018) - Institut za geološka istraživanja Zagreb, Savezni geološki zavod Beograd. SLOVENEC, DA. & LUGOVIĆ B. (2000): Ultramafic cumulate rocks from the Med- vednica Mts. ophiolite complex (Northwestern Croatia).– The central ridge of Mt. Kalnik is composed of Palaeocene carbonate breccia thrust over Neogene sedimentary rocks (ŠIMUNIĆ et al., 1981). Keywords: amphibole; crystallization; cumulates; doi; et al; fig; geol; kalnik; lugović; magmatic; mineral; mélange; oceanic; olivine; ophiolite; plagioclase; rocks; ultramafic; zone
• The characteristics of granites in the Gaofeng and Baocheng areas, Hainan Province, China: response to subduction of the Tethyan South China Sea by Xiaobo, Yuan; Nianqiao, Fang; Zhenguo, Zhang; Hailong, Dong (2019) - Earth Sci- ence Frontiers, 23/6, 107–119. GE, X.Y., LI, X.H. & ZHOU, H.W. (2003): Geochronologic, geochemistry and Sr-Nd isotopes of the Late Cretaceous mafic dyke swarmsin southern Hainan Island.– Geochimica, 32/1, 11–20 (in Chinese with English abstract). | www.geologia-croatica.hr Journal of the Croatian Geological Survey and the Croatian Geological Society Article history: Manuscript received April 23, 2019 Revised manuscript accepted July 02, 2019 Available online December 20, 2019 Keywords: Tethyan-South China Sea, Subduction, Zircon U–Pb age, Geochemistry 1. INTRODUCTION During the Mesozoic Era, there was an ancient Sea situated in the same place as the present-day South China Sea (south of Hainan Island), which experienced northward subduction during the late Mesozoic. Keywords: abstract; baocheng; characteristics; china; chinese; crust; doi; et al; gaofeng; granites; hainan; hainan island; high; island; mesozoic; rocks; sea; south; subduction; tectonic; type; zircon
• Sm-Nd geochronology and petrologic investigation of sub-ophiolite metamorphic sole from the Dinarides (Krivaja-Konjuh, Ophiolite Complex, Bosnia and Herzegovina) by Šegvić, Branimir; Slovenec, Damir; Schuster, Ralf; Babajić, Elvir; Badurina, Luka; Lugović, † Boško (2020) - Fragments of the ophiolite se- quence are also present in a mélange (Fig. 1; DIMITRIJEVIĆ & DIMITRIJEVIĆ, 1973; ŠEGVIĆ et al., 2014) consisting of a pelitic to silty sedimentary matrix which incorporated various igneous and sedimentary rocks during tectonic processes (PAMIĆ et al., 2002). Exhumed along the ancient subduction channel high-grade met- amorphic rocks were thrust onto the Adria margins along with the rest of the ophiolite sequence (PAMIĆ et al., 2002; ROBERT- SON et al., 2009a; BORTOLOTTI et al., 2013; ŠEGVIĆ et al., 2016). Keywords: age; amphibole; clinopyroxene; complex; dinarides; doi:10.1016; et al; evolution; fig; garnet; kkoc; mineral; ophiolite; pamić; plagioclase; rocks; sole; subduction; šegvić; šegvić et

• Planktonic foraminiferal biostratigraphy and lithology of the Upper Cretaceous (upper Campanian-Maastrichtian) and Palaeogene succession of the Palmyrides (Syria) by Premec-Fućek, Vlasta; Hernitz Kučenjak, Morana; Pecimotika, Gabrijela (2021) - Planktonic foraminiferal species from the upper Campanian to Maastrichtian interval inhabited a different niche in the stratified water column (ABRAMOVICH et al., 2003; HUBER et al., 1995; PETRIZZO, 2002). Planktonic foraminiferal biostratigraphy and lithology of the Upper Cretaceous (upper Campanian-Maastrichtian) ... 33 Appendix List of planktonic foraminifera species cited in the text and figure explanation, in alphabetic order according to genus: Cretaceous Archaeoglobigerina blowi PESSAGNO, 1967 Contusotruncana contusa (CUSHMAN, 1926) Contusotruncana fornicata (PLUMMER, 1931) Keywords: acarinina; assemblage; biostratigraphy; boundary; campanian; chiloguembelina; cretaceous; doi; eocene; et al; fig; foraminifera; interval; maastrichtian; middle; morozovella; oligocene; palaeocene; pearson; planktonic; species; subbotina; syria; taxa; turborotalia; upper; wade; water
• Challenges to Sustainability in the Caribbean Karst by Day, Mick (2010) - Fi gu re 1: Major locations of Caribbean karst. ACKNOWLEDGEMENT Research on Caribbean karst has been supported by grants from UWM’s Center for Latin American and Caribbean Studies, and the Mary Jo Read Bequest to the UWM Geography Department. Keywords: caribbean; change; climate; day; environmental; human; impacts; karst; sustainability; water
• Observations of stage and temperature dynamics in the epiphreatic caves within the catchment area of the Ljubljanica river (Slovenia) by Grabovšek, Franci; Turk, Janez (2010) - Croatica 188 more than a century ago, while Vetrovna Jama pri Laški Ku- kavi (Vetrovna Jama = Windy Cave) and Gašpinova Jama have been discovered and explored during the last decade. ACKNOWLEDGEMENT The authors would like to thank members of Logatec Caving Club, es- pecially Mr. Bojan VOLK, who assisted the work in Gašpinova Jama and Vetrovna Jama. Keywords: caves; jama; polje; river; stage; temperature; unica; water
• Evolution of caves in porous limestone by mixing corrosion: A model approach. by Dreybrodt, Wolfgang; Romanov, Douchko; Kaufmann, Georg (2010) - Its lower border is the dividing streamline (DS) separating phreatic water from surface water. PCO2 of phreatic water 0.0003 atm, PCO2 of surface water 0.1 atm. Keywords: aquifer; caves; change; evolution; mixing; porosity; surface; water
• New insights into the transport of sediments and microorganisms in karst groundwater by continuous monitoring of particle-size distribution by Goldscheider, Nico; Pronk, Michiel; Zopfi, Jakob (2010) - The relative increase of fi ne particles can consequently be used as an “early-warning parameter” for microbial contamination of karst spring water. Therefore, the main objectives of this study were: • to better understand the origin, transport and dynam- ics of suspended sediment particles and faecal bacte- ria in karst groundwater fl ow systems; • to test the applicability and limitations of particle counters and continuous PSD monitoring for karst hy- drogeological studies; and • to identify reliable “early-warning parameters” indi- cating the possible presence of faecal and pathogenic microorganisms in karst spring water. Keywords: karst; monitoring; particles; size; spring; turbidity; water
• Water temperature as a natural tracer – a case study of the Malenščica karst spring (SW Slovenia) by Petrič, Metka; Kogovšek, Janja (2010) - Keywords: karst spring, water temperature, recharge, Malenščica, Slovenia Water temperature as a natural tracer – a case study of the Malenščica karst spring (SW Slovenia) � Janja Kogovšek and Metka Petrič Karst Research Institute SRC SASA, Titov trg 2, 6230 Postojna, Slovenia; (kogovsek@zrc-sazu.si, petric@zrc-sazu.si) A case- study of the Malenščica karst spring in south-western Slo- venia is described here, in which water temperature was tested as a possible natural tracer. Keywords: cerknica; karst; malenščica; spring; temperature; water
• Karstic sources of water supply for large consumers in Southeastern Europe – sustainability, disputes and advantages by Stevanovic, Zoran P.; Eftimi, Romeo (2010) - Exploration and utilization of karstic waters is an ancient art in the area. The water supply from the karst is dominant along the coastal area and in the islands where karstic waters are commonly even the sole resource. Keywords: aquifers; croatica; discharge; groundwater; karst; karstic; region; sea; springs; stevanović; supply; water
• From deep-marine stratigraphic condensation to mass-transport deposition: Illyrian stepwise extension recorded in a red nodular limestone drowning sequence (Bulog Formation) of the Ravni Carbonate Ramp (Seljani area, Montenegro) by Mrdak, Milica; Gawlick, Hans-Juergen; Djerić, Nevenka; Bucur, Ioan I.; Wegerer, Eva; Đaković, Martin; Sudar, Milan (2025) - Furthermore, the recently detected stepwise deepening with at least two independent stages of creation of a horst-and-graben topography in A) the late Pelsonian, and B) around the middle/late Illyrian boundary, with time-equivalent formation of neptunian dikes and deposition of mass-transport deposits (GAWLICK et al., 2023; SUDAR et al., 2023a, b; MRDAK et al., 2024a and references therein), is still not fully understood throughout the Dinarides. Furthermore, several tectonic events, volcanism as well as biological crises affected the believed continuous deposition, resulting in cases in a very heterogenous topo- graphy and the repeated demise of shallow-water carbonate production, in cases expressed as long-lasting stratigraphic gaps (MISSONI & GAWLICK, 2012; SUDAR et al., 2013; GAWLICK et al., 2017a; MRDAK et al., 2023, 2024a). Keywords: age; bulog; carbonate; conodont; deposition; der; dikes; dinarides; et al; fig; formation; gawlick; illyrian; limestone; middle; montenegro; neptunian; paragondolella; pelsonian; ravni; red; sample; section; shallow; sudar; triassic; unit; water
• Understanding the Hydrology of Karst by Palmer, Arthur N. (2010) - Palmer.indd 143 �AB STRA CT Determining the nature of water fl ow and contaminant dispersion in karst requires far more information than can be provided by simple dye traces. (5) Volume and duration of water retained in storage betwe en infiltration events (e.g., capillary water, perched pools, etc.). Keywords: aquifer; cave; discharge; eld; groundwater; isotopes; karst; time; water
• Palaeoenvironmental and Archaeological Implications of a Sediment Core from Polje Čepić, Istria, Croatia by Balbo, Andrea L.; Andrič, Maja; Rubinić, Josip; Moscariello, Andrea; Miracle, Preston T. (2010) - In core segment S2 inclusive mean values are generally lower than those registered for core segment S1. The bottom unit D of core segment S1 could not be processed with the Mastersizer because of its detritic nature. Keywords: age; cal; core; depth; fig; holocene; istria; lake; polje; polje čepić; pollen; sediments; segment; water; years; čepić
• Planktic Foraminiferal Content in a Mature Agulhas Eddy from the SE Atlantic: Any Influence on Foraminiferal Export Fluxes? by Lončarić, Neven (2010) - Due to such a decisive role of this system in the glo- Geologia Croatica 59/1 41–50 7 Figs. 1 Tab. ZAGREB 2006 Key words: Planktic foraminifera, Southeast Atlantic, Agulhas eddies, Interocean exchange, Globorotalia menardii. Springer-Verlag, Berlin, Heidelberg, 363–410. BYRNE, D.A., GORDON, A.L. & HAXBY, W.F. (1995): Agulhas eddies: a synoptic view using Geosat ERM data.– Journal of Physical Oceanography, 25/5, 902–917. Keywords: agulhas; atlantic; eddy; fig; foraminiferal; ocean; sediment; surface; water
• Chronohorizons Based on Resistivity Curve Variations - Upper Miocene Sediments of the Ivanić Grad Formation in the Sava Depression (NW Croatia) by Vrbanac, Boris (2010) - INTRODUCTION Regionally recognisable sections of motifs (sequences of equally developed peaks) on resistivity curves of wells drilled in the Croatian part of the Pannonian Basin System were as early as the 1960’s ZAGREB 2002 Key words: Resistivity curve, Chronohorizons, Single cycle, Upper Miocene, IvaniÊ Grad Formation, Sava Depression, Croatia. Keywords: depositional; depression; formation; marls; peaks; resistivity; resistivity curve; sandstone; sediments; water
• New Stratigraphic and Palaeogeographic Results from the Palaeozoic and Early Mesozoic of the Middle Pontides (Northern Turkey) in the Azdavay, Devrekani, KŸre and Inebolu Areas: Implications for the Carboniferous - Early Cretaceous Geodynamic Evolution an by Kozur, Heinz W.; Aydin, Mustafa; Demir, Osman; Yakar, Huseyin; Goncuog Lu, M. Cemal; Kuru, Ferudun (2010) - Remnants of this Palaeotethys (MORB and OIB, as well as pelagic Carboniferous to Trias- sic oceanic sediments and Late Pennsylvanian ocean island sediments) were found in the Tavas Compos- ite nappe of the Lycian nappes (KOZUR et al., 1998; KOZUR & ŞENEL, 1999; GÖNCÜOĞLU et al., 2000; KOZUR et al., in press c). Two conflicting palaeogeo- graphic models were developed by the ŞE N G Ö R school (e.g., ŞENGÖR & YILMAZ, 1981; ŞE N G Ö R , 1984, 1985; ŞENGÖR et al., 1984; GENÇ & YILMAZ, 1995; YILMAZ et al., 1997) on one side, and OKAY and co-authors (e.g., OKAY & MOSTLER, 1994; OKAY et al., 1996) as well as ROBERTSON and co- authors (e.g., PICKETT et al., 1995; USTAÖMER & ROBERTSON, 1995, 1997, 1999; PICKETT & RO- BERTSON, 1996) on the other. Keywords: age; c o; d r; e l; e n; e o; e s; fig; formation; g e; g l; g o; group; h e; h o; küre; l l; m e; m o; middle; n d; n s; o l; o n; o r; ocean; p l; r e; r l; s t; sample; t e; t o; t r; u l; water
• Problems for Evaluation of the Scenario of the Permian -Triassic Boundary Biotic Crisis and of Its Causes by Kozur, Heinz W. (2010) - Abstract Determination of the causes o f the Permian -Triassic boundary (PTB) biotic crisis is hindered primarily by the diachronous nature of the used PTB, poor stratigraphic control of compared Upper Permian and Lower Triassic faunas, espec ially in cont inental biotopes, poor knowledge of the lower and midd le Scythian faunas from m,UlY envi­ ronments, and by interpolation of the unknown (lower and middle) Scythian diversity from the known Upper Pennian and Middle Trias­ sic diversity data in many major fossil gro ups. On the basis of the real (not interpolatcd) ext inction and recovery patterns of the major fossil groups, and with consideration of the geological phe­ nomena in the Upper Permian and Lower Triassic, a possible scenario for the PTE biotic crisis is presented. Keywords: anoxia; areas; base; beds; benthos; biotic; boreal; boundary; changes; conodont; continental; crisis; diversity; dorashamian; drop; eastern; end; event; extinction; fad; faunas; formation; genera; groups; ing; kozur; lazarus; level; low; lystrosaurus; marine; mass; middle; middle triassic; olenekian; ostracod; parvus; patterns; permian; problems; ptb; recovery; scenario; scythian; section; shallow; siberian; southern; species; taxa; tethyan; tethys; thc; time; trap; triassic; triassic boundary; tropical; upper; uppermost; volcanic; volcanism; wang; warm; water; water faunas; wignall; winter; zone
• First Evidence of Hercynian Lower Carboniferous Flyschoid Deep-Water Sediments in the Lycian Nappes, Southwestern Turkey by Kozur, Heinz W.; Senel, Mustafa; Tekin, Kagan (2010) - The Nohutluk Fomation is unconformably overlain by the shallow water Permian Arka99a Formation which is overlain by variegated shallow water limestones, mud­ stones, marl s and dolomites of Triassic age. Lower Car­ boniferous radiolarian-rich turbiditic cherty limestones and rare mudstones are overlain by shallow water lime­ stones and sandstones (upper Nohutluk Formation) of middle Visean to Bashkirian age (TEKELI et aI., 1984). Keywords: age; ankara; carboniferous; formation; kozur; limestone; nappe; permian; sequence; shallow; tavas; turkey; unit; upper; visean; water; zone; ~enel
• The Morphogenesis of Submarine Springs in the Bay of Kaštela, Croatia by Fritz, Franjo; Bahun, Stjepan (2010) - This is the rea­ SOil why most present submarine springs are situated relatively near the prcsent coastline, and also why a small number of them are pennanently active and why the largest portion of karst groundwater flowing from the mainland hinterland during dry seasons does not emerge from submarine springs but along the coastline, from brackish coastal springs, The submarine springs in the Bay of Kastela differ considerably from the described scheme of the appear­ ance of Croat ian submarine springs because their posi­ tion has not changed during the Holocene. The Morphogenesis of Submarine Springs in the Bay of Kastela, Croatia Franjo FRITZ I and Stjepan BAHUN' Key words: Submarine spring (vruJja), Morphogenesis, Hanging barrier, Coastal karst spring, Adriatic Sea, Croatia. Keywords: arbanija; bay; groundwater; karst; kastela; level; pantan; present; sea; sea level; springs; submarine; submarine springs; water; years
• lranognathus sosioensis n.sp., a New Conodont Species from the Changxingian (Late Permian) of Western Sicily by Kozur, Heinz W.; Mostler, Helfried (2010) - Acknowledgement The invest igat ion s by H. KOZUR were sponsored by the Deutsche Forschungsgemeinschaft whose help is gratcfullyacknowlcdged . Some species, like C. c/tang­ xiugensis (W ANG & WANG) and H. typicalis occur both in cold water and warm water pelagic environ­ ments. Keywords: calcarenites; changxingian; cold; conodont; deep; faunas; kozur; permian; red; sicily; slope; species; wang; water
• Prospecting for Bypassed Oil and Gas by Bassiouni, Zaki; Velić, Josipa (2010) - The noti ceable increase in prod uct ion start ing in 1990 is primarily due to the application of 3-D seismic, horizonta l wells, and othe r tec hnologies wh ich targeted bypassed oi l. The different types of bypassed oil and the means for their identification and recovery are discussed herea f'ter. Several possi­ bilities or bypassed oil were identified and ind icated by the shaded areas on the cross-section of Fig. Keywords: areas; drilling; fields; fig; gas; ion; oil; potential; production; recovery; reserves; reservoir; water; wells
• gc-38 by None (None) - Peperitic pillow basalt facies The peperitic facies developed by intrusion of lava into the soft, water soaked lime mud. Keywor ds: basalt pillow lavas, peperite, fl uid inclusions, Triassic rifting, Darnó Unit, Zagorje – Mid-Transdanubian Megaunit, Dinarides, NE-Hungary, NW-Croatia 1 Department of Mineralogy, Eötvös Loránd University, Pázmány P. sétány 1/C, H-1117, Budapest, Hungary; (gabriella-kiss@chello.hu; molnar@abyss.elte.hu) 2 Department of Geology, Faculty of Science, University of Zagreb, Horvatovac bb, Zagreb, Croatia; (lpalinkas@geol.pmf.hr) Volcanic facies and hydrothermal processes in Triassic pillow basalts from the Darnó Unit, NE Hungary Geologia Croatica 61/2–3 385–394 5 Figs. Keywords: basalt; calcite; darnó; facies; hill; hydrothermal; inclusions; lava; pillow; unit; volcanic; water
• gc-394 by None (None) - The great advantage of computer graphic enclosures is the time saving for the geologist designers during field development, easier data synthetisation, simple exchange of parts of the enclosures for different pur­ poses in future projects and the easier use of enclosures for other users. 49n SATURATION c=J GAS (SEDIMENTS) ~ GAS (BASEMENT) c::::::::J OIL (SEDIMENTS) c::::J OIL (BASEMENT) Keywords: oil; water
• gc-410 by None (None) - For this reason, the Sc and M element of ' -/. sosioensis arc either identical with those of H. cr. typicalis or not present in sample PK 2. H. postparVlfs KOZUR evolved from H. parl'lfS par .1 (KOZUR & PJATAKOVA) (~f-I. par,,s, mor­ photype 2) by separation of the posterior dentieles of the Pa clement in size and inclination from the erect anterior denticies. Keywords: apparatus; appearance; arc; bar; base; bears; beds; blade; boundary; changxingian; china; clarkina; clements; conodonts; cup; cusp; denticles; element; faunas; fig; figs; forms; group; h. parvus; hilldeodlls; hindeodus; isarcica; isarcicella; kozur; lowermost; meishan; mostler; n.sp; n.subsp; occurrence; orchard; pa element; pars; parvlis; parvus; permian; posterior; present; remarks; rep.-no; sample; section; sicily; south; species; specimen; sweet; thc; thi; triassic; type; typicalis; upper; view; wang; water; yin; zhang; zone
• Upper Turonian–Santonian slope limestones of the Islands of Premuda, Ist and Silba (Adriatic Coast, Croatia) by Moro, Alan; Ćosović, Vlasta (2012) - 1a– Pelagic limestones (LF 2), b– Laminated pe- lagic limestones (LF 1), c– Intercalations of bioclastic limestones within laminated pelagic limestones (LF 3), 2– Bioclastic limestones with bioclasts (a– fragments, b– rudist shells) and lithoclasts (c) (LF 3), 3– Slump forms, 4 – Slope apron facies with blocks of laminated pelagic limestones, 5–Structural type: Towards the proximal part of the slope (Ist succession) (Pl. 2, figs. 4 & 9; Pl. 3, figs1, 2, 10 & 11) they appear commonly as intercalations within pelagic limestones and locally within laminated pelagic limestones. Keywords: cretaceous; fig; ist; limestones; platform; premuda; profile; shallow; silba; slope; water
• Systematics and biostratigraphy of Oligocene (Rupelian-Early Chattian) foraminifera from lagoonal-very shallow water limestone in the eastern Sivas Basin (central Turkey) by Sirel, Ercument; Erdem, Nazire Ozgen; Kangal, Ozgen (2013) - The Eğribucak section, located near the Eğribucak vil- lage (E of Sivas) (Fig. 2), is the type locality of several new foraminiferal taxa, namely, the new miliolid genus Sivasina n. gen. (type species S. egribucakensis n. gen. n. sp.) and the new peneroplid species Peneroplis fl abelliformis n. sp., Co- scinospira elongata n. sp. and C. sivasensis n. sp. S. egribu- cakensis n. gen. n. sp. and P. fl abelliformis n. sp. are recog- nized from the Rupelian-early Chattian (SBZ 21, 22) Croatica 86 blage, that consists of P. oligocenica n. sp., P. minuta n. sp., P. diyarbakirensis, P. minimus, A. kirkukensis, A. brunni, S. egribucakensis n. gen. n. sp. and Heterillina sp. of Rupelian age. Keywords: chambers; chattian; fi gs; fig; label; n. sp; paratype; rupelian; section; shallow; si̇rel; species; water
• Bauxites : Feedbacks of System Earth at Greenhouse times by Mindszenty, Andrea (2016) - Key: 1 - continental crust, 2 - carbonate platforms/open shelves, 3 - pelagic/hemipelagic basins, 4 - terrige- neous shelves, 5 - deformed belts and ophiolites, 6 - oceanic crust anjd sediments, 7 - Tethyan karst baux- ites (insert: world bauxites karst+laterite), AM - Armorican Massif, MC -Massif Central, BM - Bohemian Massif, EA - Eastern Alps, Tr - Transdanubian range, MP -Moesia, hE -hellenids, hK - Dinaric high Karst, AP -Apulia, LA - Latium-Abruzzi, LC - Campania-Lucania, CS - Corsica-Sardinia, Py - Pyrenees, LP - Languedoc-Provence, IBM - Iberian Massif, 30o - estimated paleolatitudes (based on PArrISh et al., 1982, MárToN & MárToN, 1985 and SCLATEr et al., 1977). Sci., 304, 397−437. doi: 10.2475/ajs.304.5.397 BErNEr, r.A. (1991): A model for atmospheric Co2 over Phanerozoic time.− amer. Keywords: anoxic; atmospheric; bauxites; bárdossy; carbon; climate; cretaceous; cycle; doi; earth; et al; global; greenhouse; mindszenty; sediments; times; water; weathering
• Quaternary Depositional Environments in the Vrgoračko Polje/Lake (SE Croatia) by Posilović†, Hrvoje; Galović, corresponding author, Lidija; Stejić, Petar; Pandurov, Mihajlo; Gajić, Rodoljub (2018) - doi: 10.1016/B978-0-444-53643-3.00056-X ZOLITSCHKA, B., FRANCUS, P., OJALA, A.E.K. & SCHIMMELMANN, A. (2015): Varves in lake sediments – a review. G eo lo gi a C ro at ic a Geologia Croatica 71/3152 nated by surrounding clay sediments, giving them an orange margin. Keywords: brown; carbonate; chalk; clay; dark; doi; et al; facies; fig; lacustrine; lake; light; polje; sediments; vrgoračko; vrgoračko polje; water; yellowish; yellowish brown
• Protecting the Karst Te Waikoropupū Springs in New Zealand by Mead, Donald James (2018) - The impacts of increasing cow numbers are recognised as a major freshwater environmental problem in many parts of New Zealand (SCARSBROOK et al., Protecting the karst Te Waikoropupū Springs in New Zealand Donald J Mead 26 Gibbs Road, Collingwood, 7073, New Zealand; (don.mead@gmail.com) doi: 10.4154/gc.2018.08 Abstract The sacred Te Waikoropupū Springs are New Zealand’s largest, have some of the clearest fresh- water worldwide and are a major tourist attraction. Te Waikoropupū Springs are the largest freshwater springs in New Zealand with an average flow of 13.3 m3/sec and they have some of the clearest water in the world with a black-disc visibi- lity of 63 m (STEWART & THOMAS, 2008; DAVIES-COL- LEY & SMITH, 1995). Keywords: aquifers; freshwater; management; new; springs; takaka; waikoropupū; water; williams; zealand
• Study of Aqueous and Non-Aqueous Phase Liquid in Fractured Double-Porosity Soil Using Digital Image Processing by Kok Foong, Loke; Abd Rahman, Norhan; Nazir, Ramli; W. Lewis, Roland (2018) - Soil sample 1 before vibration process. Soil sample 1 after vibra- tion process with fracture. Keywords: column; digital; et al; image; liquid; migration; napl; porosity; porosity soil; sample; soil; soil sample; water
• Vibration effect influence upon non-aqueous phase liquid migration in double-porosity soil by Abd Rahman, Norhan; Foong, Loke Kok; Nazir, Ramli; Lewis, Roland W (2018) - Meanwhile, the pri- mary porosity and secondary porosity continuums concept rep- resents double porosity soils that consist of inter-aggregate and intra-aggregate pore matrix blocks, respectively, with different hydraulic properties embedded in a network of interconnected Article history: Manuscript received January 06, 2018 Revised manuscript accepted June 10, 2018 Available online October 12, 2018 Keywords: vibration, laboratory experiment, NAPLs migration, aggregate kaolin, image analysis method G eo lo gi a C ro at ic a Geologia Croatica 71/3164 fractures (LOKE et al., 2017). This study proposed a new model concept with soil porosity that includes features from the three continuums of fracture porosity, primary porosity, and sec- ondary porosity (based on a literature review). Keywords: column; flow; image; lnapl; lnapl migration; migration; porosity; porosity soil; sample; soil; soil sample; surface; vibration; water
• Chemical, mineralogical and structural features of native and expanded perlite from Macedonia by Reka, Arianit A.; Pavlovski, Blagoj; Lisichkov, Kiril; Jashari, Ahmed; Boev, Blažo; Boev, Ivan; Lazarova, Maja; Eskizeybek, Volkan; Oral, Ayhan; Makreski, Petre (2019) - The volume of 2.5 ml of native perlite versus the volume of 50 ml of the expanded perlite. XRPD analysis of native perlite (top) and expanded perlite (bottom). are represented by α-quartz (26.67°) and cristobalite (21.94°). Keywords: analysis; chemical; et al; fig; glass; macedonia; mass; native; perlite; water
• A new numerical method for the analysis of monolithic seepage problems with complex drainage systems in a groundwater recharge area for a hydropower station in China by Jun, Yan; Si-hong, Liu; Ying-qi, Wei; Song-li, Jin; Hong, Cai; Jian-zhang, Xiao (2019) - Drainage holes of array 1 are drilled in upward direction from the roof of drainage gallery 1, while drainage holes of array 2 and array 3 are drilled between the upper gallery and the lower gallery. doi: 10.1002/nme.1345. ZHOU, C.B., XIONG, W.L. & LIANG, Y.G. (1996): A new method for the solution un- confined seepage field.– Journal of Hydrodynamics, 10/1, 528–534. ZHU, Y.M. (1997): The equivalent nodal flux method for the calculation of Darcy flow.– Journal of Hohai University, 7/1, 105–108. ZHU, Y.M. & SU, B.Y. (1991): Procedure of virtual flux for seepage free surface with fixed mesh.– Journal of Hohai University, 5/2, 113–117. ZHU, Y.M. & ZHANG, L.J. (1997): Solution to seepage field problem with the technique of improved drainage substructure.– Journal of Geotechnical Engineering, 19/1, 69–76. Keywords: boundary; dam; domain; drainage; drainage holes; element; free; method; seepage; seepage surface; surface; water; waterhead

• The origin of a complex breccia body within the Upper Cretaceous/Early Eocene succession on Pag Island (Karst Dinarides, Croatia): karstic dissolution and collapse or dilational faulting and collapse origin? by Kurtanjek, Dražen ; Bucković, Damir; Tibljaš, Darko; Cvetko Tešović, Blanka (2022) - These categories include: (1) crackle breccia when the rock is highly fractured with thin fractures separating breccia clasts (Fig. 3D); (2) mosaic brec- cia; when displacement between clasts is greater and some of the clasts are rotated (upper part of Fig. 3E); this type includes both matrix-free and matrix-rich varieties. (D) Crackle breccia – highly fractured host rock with thin fractures separating breccia clasts. Keywords: body; breccia; breccia body; calcite; carbonate; clasts; collapse; cretaceous; doi; eocene; fault; fig; fragments; geol; host; matrix; origin; rock; void
• Ichnotaxonomy of microboring traces in marine aphotic depths by Golubić, Stjepko; Radtke, Gudrun; Hook, James E.; Campbell, Susan E. (2024) - A fan-shaped sporangial cavity of S. papilio trace with radiating tunnels, distributed on the interior surface of a cracked pteropod shell. ACKNOWLEDGMENT We thank the National Science Foundation for the earliest sup­ port of this work through the National Science Foundation (NSF) Grant EAR­8306179 (1980–1982) and NSF Grant EAR 8107686 (1983–1984) to S. GOLUBIC and S.E. CAMPBELL, as well as a National Aeronautics and Space Administration (NASA) Keywords: bioerosion; branches; branching; campbell; carbonate; clava; complex; deep; depths; diameter; doi; endoliths; et al; euendolithic; feature; fig; figs; filaments; fossil; golubic; golubic et; holotype; hook; ichnospecies; interior; isp; marine; microboring; new; nov; organisms; orthogonum; pteropod; radtke; resin; saccomorpha; scolecia; sea; shell; size; sporangial; study; substrate; substrate surface; surface; swellings; traces; tubular; tunnels; wisshak
• Biostratigraphy of Turonian to (?)Coniacian Platform Carbonates: A Case Study from the Island of Cres (Northern Adriatic, Croatia) by Korbar, Tvrtko; Husinec, Antun (2003) - In general, this distribution represented by radiolitids dominating hippuritids in more internal peritidal cycles, seems to be typical of the central/southern Tethyan carbonate platforms (CARANNANTE et al., 2000; STÖSSEL & BERNOULLI, 2000; MORO et al., 2002; KORBAR, 2003). It is built up of predominantly Cretaceous carbonates, although there are some minor scattered outcrops of Palaeogene deposits (POLŠAK, 1967a; MAGAŠ, 1968; MAMU- ŽIĆ, 1968; ŠIKIĆ et al., 1969). Keywords: adriatic; carbonate; castro; coniacian; cres; cretaceous; croatia; fig; hippurites; island; jelaska; platform; rudists; turonian
• Depositional Environment of Coral–Rudist Associations inthe Upper Cretaceous Cardenas Formation (Central Mexico) by Schafhauser, Armin A.; Goetz, Stefan A.; Baron-Szabo, Rosemarie A.; Stinnesbeck, Wolfgang A. (2010) - So rudist reefs of the Cardenas Formation flourished in times of low sediment input during transgressive phases. Institute of Geology, Zagreb, 67. SCOTT, R.W. (1995): Cretaceous rudists of Guatemala.– Revista Mexicana de Ciencias Geológicas, 12/2, 294–306. SCOTT, R.W., FERNANDEZ-MENDIOLA, P.A., GILI, E. & SIMO, A. (1990): Persistence of coral–rudist reefs into the Late Cretaceous.– Keywords: carbonate; cardenas; coral; cretaceous; fauna; fig; formation; marls; mexico; radiolitid; reefs; rudist; rudist reefs; sandstones; section; sediments; units; upward
• Carbonate Sedimentation Rates Today and in the Past: Holocene of Florida Bay, Bahamas, and Bermuda vs. Upper Jurassic and Lower Cretaceous of the Jura Mountains (Switzerland and France) by Strasser, Andre; Samankassou, Elias (2010) - Petrol., 37, 633–648. STRASSER, A. (1984): Black-pebble occurrence and genesis in Holocene carbonate sediments (Florida Keys, Bahamas, and Tunisia).– J. Sed. HALLOCK, P. (1981): Production of carbonate sediments by selected large benthic foraminifera on two Pacific coral reefs.– J. Sed. Keywords: accumulation; carbonate; cores; facies; fig; florida; geol; holocene; level; past; rates; samankassou; sea; sediment; sedimentation; sequences; shallow; time
• Geochemical Baseline Mapping of Soils Developed on Diverse Bedrock from Two Regions in Croatia by Miko, Slobodan; Halamić, Josip; Peh, Zoran; Galović, Lidija (2001) - In order to trace the increasing human contribution to Geochemical Baseline Mapping of Soils Developed on Diverse Bedrock from Two Regions in Croatia Slobodan MIKO, Josip HALAMI∆ , Zoran PEH and Lidija GALOVI∆ overall contamination of the planet, particularly by the chemical elements harmful to health, it is necessary to determine the natural content of major and trace ele- ments in soils on the regional scale. 61Miko, HalamiÊ, Peh & GaloviÊ: Geochemical Baseline Mapping of Soils... soils from the Pannonian part of Croatia is 424 mg/kg, whereas from southern Dalmatia is 324 mg/kg. Keywords: carbonate; concentrations; contents; croatia; dalmatia; data; distribution; elements; mean; nw croatia; peh; plate; soils; southern
• Stable Isotope Event Markers Near the Permo-Triassic Boundary in the Karavanke Mountains (Slovenia) by Dolenec, Tadej; Lojen, Sonja; Busen, Stanko; Dolenec, Matej (2010) - Organic carbon isotope values were calibrated using the IAEA-CH-7 standard with a δ1 3C value of -3 1 .8‰ on the PDB scale. ZAGREB 1999 Key words: Permo-Triassic boundary, Karavanke Mountains, Slovenia, Oxygen, Carbonate carbon, Organic carbon stable isotopes. Keywords: boundary; carbon; carbonate; isotope; karavanke; permian; triassic
• Alveolinas From the Bunić Section (Lika, Croatia) by Drobne, Katica; Trutin, Mladen (2010) - canavarii CHECCHIA-RISPOLl, A. ruetimeyeri HOTTINGER, A. rectiangula DROBNE and others. sections under the specific designation: A. histri­ ca his/rica DROBNE and A. h. septentrionalis DROB­ NE Keywords: adriatic; carbonate; cuisian; drobne; eocene; fig; herak; margin; middle; platform; section; species; tectonic
• Decastronema barattoloi (DE CASTRO), characteristic fossil of the Palaeocene and the Eocene peritidal sediments from the Adriatic carbonate platform by Ćosović, Vlasta; Drobne, Katica; Ogorelec, Bojan; Moro, Alan; Koić, Mladen; Šoštarko, Ivan; Tarlao, Alceo; Tunis, Giorgio (2008) - Shortly after spec- imens of A. barattoloi were described in sediments of Mt. Mutria (DE CASTRO, 1989), this species was recognized in sediments from the central part of the AdCP, (Ravni kotari re- gion, DROBNE et al., 1991; Fig. 1). Alternatively, DROBNE and co-workers (DROB- NE, 2003; DROBNE & OGORELEC, 2006; DROBNE et al., 2008) defi ned a model where four biosedimentary zones (Bio- sZ1 – BiosZ4; Fig. 2) followed stepwise, one after another, from the Late Cretaceous to Middle Eocene (Lutetian/Barto- nian boundary). Keywords: adriatic; age; barattoloi; carbonate; decastronema; drobne; eocene; et al; palaeocene; platform; section; sediments
• gc-469 by None (None) - i karbonati središnjeg dijela Dinarida su sedimenti taloženi u evaporizacijskim i u morskom zaštićenom plićaku (nije prikazano na slici). Keywords: anhidrita; anhydrite; breccias; carbonate; cavity; central; coastal; conditions; cycle; depositional; dinarides; dolomite; environments; evaporite; facies; fig; fragments; general; gips; gypsum; hydration; ili; laminae; marine; origin; permian; sabkha; sediments; slika
• Geochemical characteristics of different iron ore types from the Southern Tomašica deposit, Ljubija, NW Bosnia by Garašić, Vesnica; Jurković, Ivan (2012) - TCOR TMIC AD-2 mineral/ rock compact limonite pulverized limonite limestone carbonate shale ankerite ankerite ankerite ankerite siderite siderite siderite white gray fi ne to coarse grained white coarse grained white coarse grained dark fi ne grained red coarse grained dark fi ne grained yellow coarse grained   ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm La 0.10 3.60 27.3 1.70 16.30 1.40 <0.10 <0.10 1.20 2.20 2.60 1.80 Ce 0.10 5.50 42.6 2.40 27.70 3.90 0.40 0.10 2.30 4.10 5.10 3.80 Pr 0.02 0.75 6.16 0.44 3.55 0.86 0.14 0.06 0.44 0.75 0.86 0.63 Nd 0.30 3.20 22.3 1.80 13.80 4.60 1.00 0.80 2.40 3.10 4.40 2.90 Sm 0.05 0.81 4.79 0.48 2.57 1.91 0.62 1.57 0.87 0.72 0.95 0.90 Eu 0.02 0.61 1.57 0.21 0.87 1.72 0.50 1.91 0.65 0.51 0.74 0.99 Gd 0.05 0.96 3.97 0.67 2.54 2.58 0.81 2.87 1.19 0.67 0.85 0.88 Tb 0.01 0.18 0.63 0.10 0.40 0.45 0.15 0.55 0.18 0.12 0.15 0.13 Dy 0.05 1.06 3.64 0.58 2.14 2.31 0.77 3.09 1.01 0.75 0.97 0.67 Ho 0.02 0.25 0.73 0.13 0.43 0.47 0.15 0.59 0.19 0.17 0.22 0.14 TCOR TMIC AD-2 mineral/ rock compact limonite pulverized limonite limestone carbonate shale ankerite anker- ite ankerite ankerite siderite siderite siderite white gray fi ne to coa rse grai ned white coarse grained white coarse grained dark fi ne grained red coarse grained dark fi ne grained yellow coarse grained   ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm Sc 1.0 2.0 12.0 <1.0 5.0 <1.0 <1.0 <1.0 <1.0 <1.0 <1.0 1.0 Ba 1.0 201.0 227.0 26.0 140.0 24.0 5.0 8.0 18.0 17.0 21.0 44.0 Be 1.0 1.0 2.0 <1.0 <1.0 <1.0 <1.0 <1.0 <1.0 <1.0 <1.0 <1.0 Co 0.2 2.7 18.1 0.2 25.9 2.7 0.5 0.8 4.1 3.6 5.6 11.7 Keywords: ankerite; carbonate; coarse; compact; grained; limonite; ore; ppm; ree; sample; shale; siderite; tomašica
• A novel concept in the growth and design of anhydrous carbonate minerals: nano-scale aggregation mechanisms by Sondi, Ivan; Škapin, Srečo D.; Jurina, Irena; Slovenec, Damir (2011) - Zagreb 2011 Geologia CroaticaGeologia Croatica 1. INTRODUCTION Anhydrous carbonate minerals are frequently found in Na- ture, commonly occurring as the main mineral constituents in rocks and sediments, and as the most common constitu- ents of the bio-inorganic structures of the skeletons and tis- sues of many mineralizing organisms (TUCKER & WRI- GHT, 1990; FLÜGEL, 2004; SONDI & JURAČIĆ, 2010; SONDI et al., 2011). (Figure adapted from SONDI et al., 2011). Keywords: aggregation; carbonate; formation; growth; mineral; particles; sondi
• Onset of an Aptian carbonate platform overlying a Middle-Late Jurassic radiolaritic-ophiolithic mélange in the Mirdita Zone of Albania by Schlagintweit, Felix; Gawlick, Hans-Jürgen; Lein, Richard; Missoni, Sigrid; Hoxha, Lirim (2011) - After erosion of the Kurbnesh platform, the ?Late Berriasian-Valanginian Figure 1: A simplifi ed tectonic map of Albania (after NOWACK, 1928; XHO- MO et al., geological map of Albania 2002) and the study area. The total taxon range should be restricted to the lowermost part of the Early Aptian (Bedoulian) (e.g., SCHRO- EDER, 1964, fi g. 1; SCHROEDER et al., 2010, fi g. 3). Keywords: albania; aptian; carbonate; et al; fig; jurassic; late; platform; schroeder; section; zone
• Specific aspects of engineering-geological models in Croatian karst terrain by Pollak, Davor; Navratil, Dražen; Novosel, Tomislav (2013) - There are numerous examples to support the thesis of the influence of depositional and diagenetic conditions on the rock material and rock mass engineering properties. Once com- pleted, this leads to the most accurate determination of the rock material and rock mass engineering properties and pre- diction of post-engineering behaviour. Keywords: carbonate; carbonate rock; croatian; data; discontinuity; engineering; frequency; geological; karst; mass; model; properties; rock; rock mass; rqd; tunnel; weathering
• The Paleozoic record of Thaumatoporella PIA, 1927? by Schlagintweit, Felix; Hladil, Jindrich; Nose, Martin; Salerno, Carlo (2013) - In the latter case, thaumatoporellacenas might have survived the end-Permian mass-extinction (e.g., KNOLL et al., 2007; BOTTJER et al., 2008; SAHNEY & BENTON, 2008) and could then be considered as a long- term refugia species (e.g., HARRIES et al., 1996). Upper Cretaceous of Guatemala), Messopotamella an­ gulata (DRAGASTAN et al., 1985: Keywords: algae; birina; bisphaera; carbonate; castro; cretaceous; cribrosphaeroides; croatica; devonian; doi; et al; facies; fig; foraminifera; forms; geologia; incertae; italy; mesozoic; middle; palaeozoic; pia; platform; pores; schlagintweit; section; sedis; specimens; thaumatoporella; thaumatoporellaceans; thin; uslonia; vachard; vermiporella; wall
• Dinosaur footprints in the Upper Hauterivian deposits of the Palud Bay in Istria, Croatia by Mezga, Aleksandar; Cvetko Tešović, Blanka; Pretković, Vedrana; Jovanović, Nina; Bajraktarević, Zlatan (2015) - Keywords: Dinosaur footprints, Sauropods, Lower Hauterivian, Palud, Istria, Croatia Cretaceous strata of the Palud site on the Istrian penin- sula are part of the Adriatic-Dinaridic Carbonate Platform succession (ADCP – also referred to as the Adriatic Carbon- ate Platform, see discussion in VLAHOVIĆ et al., 2005). Dinosaur footprints in the Lower Hauterivian deposits of Palud Cove in Istria, Croatia  Aleksandar Mezga, Blanka Cvetko Tešović, Vedrana Pretković, Nina Jovanović and Zlatan Bajraktarević Department of Geology and Paleontology, Faculty of Science, Horvatovac 102a, Zagreb, Croatia; (amezga@geol.pmf.hr) doi: 10.4154/gc.2015.08 Geologia CroaticaGeologia Croatica Geologia Croatica 68/2Geologia Croatica 114 range from the late Middle Jurassic to the Eocene (VELIĆ et al., 2003). Keywords: carbonate; cretaceous; croatia; dalla; dinosaur; footprints; istria; palud; vecchia
• Geochemistry of Lower Palaeogene bauxites – unique signature of the tectonostratigraphic evolution of a part of the Croatian Karst by Peh, Zoran; Kovačević Galović, Erli (2016) - DF1 and DF2 together account for more than 94% and almost 93% of the total between-group difference in ILPB and LPB models, respectively, allowing the third one to be easily disregarded. LPB model revisited – the CoDa approach Previous investigation of Lower Palaeogene bauxites revealed an exceptional role for Cr in their disposition over the Dinaric karst (KOVAČEVIĆ GALOVIĆ et al., 2012). Keywords: adcp; adriatic; analysis; bauxites; carbonate; cretaceous; data; et al; forebulge; formation; galović; geochemical; groups; ilpb; istrian; karst; kovačević; lpb; model; palaeogene; platform
• Hydrodynamic and hydrochemical conditions at the groundwater source Pašino vrelo, with a focus on its development on its development by Larva, Ozren; Marković, Tamara; Mraz, Vinko (2010) - However, at times of low waters, the isotopic composi- tion of spring waters is infl uenced by groundwater from the lithothamnium limestones. Poorer oxygen saturation of well waters is a consequence of the consumption of oxygen in the alluvial aquifer for differ- ent chemical reactions, such as the oxidation of organic mat- ter, mineral wear, nitrogen transformation processes, etc. Keywords: aquifer; bojanića; carbonate; conditions; croatica; groundwater; groundwater source; pašino vrelo; pumping; source; spring; sunja; waters; wells

• The Žune Ba-F epithermal deposit: Geophysical characterization and exploration perspective by Orešković, Jasna ; Milošević, Aleksej; Kolar, Saša; Borojević Šoštarić, Sibila (2023) - The de- posit is clearly visible on both profiles (ERT-1 and ERT-4) as a shallow high resistivity anomaly and in resistivity models it is defined with 5·103 Ωm. Resistivity models are on the left and inversion of calculated resistivity pseudosections on the right. Keywords: barite; cut; data; deposit; fig; fluorite; inversion; mining; model; ore; profile; resistivity; žune
• Continuous Wavelet Transformation to Quantify small-scale Cycles of Petrophysical Properties; a New Approach Applied in a Potential Disposal Repository of Nuclear Waste, SW Hungary by Mohammad Abutaha, Saja; Geiger, Janos; Fedor, Ferenc; Gulyás, Sándor (2023) - In our case, wavelet coefficients of voxel­porosity lead the rock­forming com- ponents series on positive lags. 6A, the wavelet power spectrum graph (scalogram) plots the absolute value of wavelet coefficients. Keywords: albite; analysis; claystone; coefficients; components; core; data; doi; et al; fig; formation; fragments; frequency; porosity; rock; sample; scale; series; signal; siltstone; time; transform; wavelet; wavelet coefficients
• Qualitative–Quantitative Analyses of the Influence of Depth and Lithological Composition on Lower Pontian Sandstone Porosity in the Central Part of Bjelovar Sag (Croatia) by Malvić, Tomislav; Velić, Josipa; Peh, Zoran (2010) - Input data were porosity values measured in verti- cal cores, performed in the INA-Naftaplin laboratory and noted in well files. 1 INA–Industry of Oil Plc. (Naftaplin), Šubićeva 29, HR-10000 Zagreb, Croatia; e-mail: tomislav.malvic@ina.hr 2 Faculty of Mining, Geology and Petroleum Engineering, University of Zagreb, Pierottijeva 6, HR-10000 Zagreb, Croatia; e-mail: jvelic@rgn.hr 3 Institute of Geology, Sachsova 2, HR-10000 Zagreb, Croatia; e-mail: zpeh@igi.hr Abstract Results of several tests (porosity–depth graphic relation, t-test, F- test, Pearson’s R), were used to analyse and interpret the regularity in porosity values of Lower Pontian oil-bearing sandstones from the central part of Bjelovar sag. Keywords: ciglena; compaction; cores; data; depth; mean; member; pepelana; poljana; porosity; sandstones; values; velika
• System Architecture for 3D Gravity Modelling by Šumanovac, Franjo A.; Ritsema, Ipo L.; Bril, Bert H. (2010) - CORDELL, L. & HENDERSON, R.B. (1968): Iterative three-dimensional solution of gravity anomaly data using a digital cOIllputer.- Geophysics, 33, 596-60l. GOTZE, Il. -J. & LAHMEYER, B. (1988): Application of three-dimensional intcractive modeJing in gravity and magnetics.- Geophysics, 53, 1096-1108. GRANSER, H. (1987): Three-dimensional inlerpreta­ tion of gravity data from scdimcntary basins using an exponential density-depth fUllclion.- Geophysica! Keywords: anomaly; architecture; body; cases; complex; data; dome; ewing; fig; gravity; inversion; ion; method; model; modelling; salt; software; surface; thc; tion
• Hydrocarbon Reserves Replacement· Methods and Expenditures by Bauk, Antun (2010) - Acquisit ion or reserves as a method of reserve replacement is st ill unknown in Croati a, but prccisely thi s met hod sho uld provide a so lution to the current s itu a­ tion. The results of the period from 1980- 1984 arc similar, in fact the ove rall results of reserve replacement by all methods arc the lowest - only 7.1 %. Keywords: arc; data; development; exploration; field; gas; ina; methods; oil; period; production; recovery; replacement; reserves; reservoir; results; revision; table; total; year
• Seismic Line Calibration - A Main Reference for the Rational Exploration and Development of Very Complex Oil and Gas Fields and Reservoirs (Bizovački Čret Case Study) by Gaćeša, Slobodan A.; Mesić, Ivan (2010) - The best matching of the synthetic seismogram and seismic line was achieved by sliding the synthct­ ic seismogram from 132 elF on seismic line to 142 elF. Results indicate that slich Key seismic line (a reference) may be use ful as an entry for three-dimensional (3~) seismic surveys. Keywords: bizovac; data; field; fig; line; reservoir; seismogram; synthetic
• Critical Geological Parameters in Feasibility Studies of Exploration Projects by Kolbah, Slobodan (2010) - Economic appra isa l wil l a lso take into account concession term s, ri sk s preading , politi cal risks and poss ibl e technologica l improve ments. CroatiCKeywords: data; exploration; ing; oil; pannonian; parameters; project; reservoir
• gc-390 by None (None) - However, many seismic am pli­ Il1de anomal ies have nOI been call sed by gas accumulat ions, but they arc re l:lled 10 lithological changes. The difference between gas accumulat ions and lithological changes can be identified by the AVO analysis inver­ sion or se ismic data, and this also contributed to the more rational cOlllouring of the gas accumulation and to the well location. Keywords: amplitude; arc; avo; data; fig; gas; ing; inversion; ion; log; methods; rap; section; seismic; spot; stack; synthetic
• gc-393 by None (None) - Land sat T M inte r­ pre tation of the area on-shore, toge ther with the inte r­ pre tation of off-shore seism ic data , resul ted in the con­ struc tion of new structural map of the exploration area. tudy of the lates t geological data from the Ka mali block and other relevant areas is based on the follow ing e lements: - slnHig raphi c evolution linked to structural history; - definiti on of potential source rocks , their stratigraphic and geographic exten t; - palac: ol cc lon ic contro l of variolls depositional envi ­ ronm ent s . Keywords: data
• gc-395 by None (None) - However, together with the undisputed qualities or geophysical techniques, it is ve ry often forgotten that such data, which are to be used in thc correlation ancimocielling of a given geolog­ ical object (depression, fi e ld), must be calibratcd with the data ga ined by petrographical, sed imentological, and also, biostratigraphical analyses and interpretations (LUCIC & KRIZMANIC. 1993). How­ ever, biostratigraphical data are more valid when utilised in conjunction with other related sciences (biol- INA -Naftaplin. Keywords: arc; biostratigraphy; data; fucek; oil; premec
• gc-467 by None (None) - This study shows a neural network methodology which can handle simultane- ously more point data and even join more attributes, or prop- erty of data points. The main goal of SOM is to represent data points with fewer representatives preserving the original topology (JOHANNSON, 2003). Keywords: case; clustering; clusters; data; kohonen; map; network; pattern; points; set; som
• Stochastic simulations of dependent geological variables in sandstone reservoirs of Neogene age: A case study of Kloštar Field, Sava Depression by Novak Zelenika, Kristina; Malvić, Tomislav (2011) - A comparison of Figures 5 and 7 shows thickness values mapped by the SGS and SIS methods, respectively. Croatica 182 Figure 14: Histogram of thickness values as calculated by SGS (left) and by SIS (right). Keywords: data; figure; malvić; porosity; realizations; reservoir; simulations; sis; stochastic; thickness; values
• Application of Neural Networks in Petroleum Reservoir Lithology and Saturation Prediction¸ by Cvetković, Marko; Velić, Josipa; Malvić, Tomislav (2009) - Keywords: Kloštar fi eld, neural network, prediction, sandstone, hydrocarbon saturation, Croatia Application of neural networks in petroleum reservoir lithology and saturation prediction � Marko Cvetković1, Josipa Velić1 and Tomislav Malvić1,2 1 Department of Geology and Geological Engineering, Faculty of Mining, Geology and Petroleum Engineering, Pierottijeva 6, 10000 Zagreb, Croatia; (marko.cvetkovic@rgn.hr) 2 Development Department, Oil & Gas Exploration and Production, INA-Industrija nafte d.d., Šubićeva 29, 10000 Zagreb, Croatia; (tomislav.malvic@ina.hr) doi: 10.4154/gc.2009.10 Geologia Croatica 62/2 115–121 6 Figs. At present, this study represents the best and most useful application of neural networks in the Croatian part of the Pannonian Basin. Keywords: analysis; data; klo; lithology; network; neural; prediction; sandstone
• The evolution of the Čanište epidote-bearing pegmatite, Republic of Macedonia: evidence from mineralogical and geochemical features by Strmić Palinkaš, Sabina; Bermanec, Vladimir; Palinkaš, Ladislav A.; Boev, Blažo; Gault, Robert A.; Prochaska, Walter; Bakker, Ronald J. (2012) - Bulk fluid density, estimated from fluid inclusion data, spans from 0.931 to 0.951 g/cm3. The crystallization evolution of the Čanište epidote- bearing pegmatite, is reconstructed using thermodynamic mineral equilibria and fluid inclusion data. Keywords: d.l; data; doi; epidote; fig; fluid; inclusions; microcline; mineral; pegmatite; quartz; temperature; zone; čanište
• Comment on the paper "Definition of the river Gacka springs subcatchment areas on the basis of hydrogeological parameters" by Lukač Reberski et al., published in Geologica Croatica 66/1, 39–53 (2013) by Roller-Lutz, Zvjezdana; Hunjak, Tamara; Lutz, Hans O. (2013) - Therefore, the majority of data points are actu- ally located slightly above the correct LMWL. (in the following referred to as paper I) Keywords: data; paper; spring
• Traces of drilling predation in the Badenian Mollusks from the Rakovica stream (Belgrade, Serbia) by Ganić, Meri; Radović, Predrag; Rundić, Ljupko; Bradić, Katarina; Knežević, Slobodan (2016) - Among bivalves, the Veneridae show similar differences (DF in Rakovica sample is 11.58%, com pared to 7.6% in Central Paratethys). These differ- ences could be due to the fact that samples come from different stratigraphic settings: the Rakovica sands is Upper Badenian, the Central Paratethys sample comes from the Karpatian – Badenian, Paratethys sample is from Burdigalian – Serravallian, and Boreal, Southeastern North Atlantic and US Atlantic Coast are from Mid- dle – Late Miocene. Keywords: assemblage; badenian; belgrade; central; data; drilling; gastropods; kowalewski; miocene; paratethys; predation; predator; prey; rakovica; sample; study; zuschin
• Statistical and geostatistical study of Rn and hydrocarbon components of a soil gas monitoring system: an application to surface hydrocarbon exploration by Geiger, Janos; Jakab, Noémi; Csökmei, Bálint; Horváth, Zsolt; Gellért, Balázs (2016) - From the positive verification, regions with a high probability positive anomaly of factor scores, but without any reservoir counterparts may be suggested as targets for further surface hydro- carbon exploration. The coordinates of this factor space are called factor scores. Keywords: analysis; components; data; distribution; factor; factor scores; fig; gas; hydrocarbon; map; migration; model; probability; process; reservoirs; scores; simulation; soil; surface; variance
• Application of the deterministical and stochastical geostatistical methods in petrophysical modelling - a case study of Upper Pannonian reservoir in Sava Depression by Novak Zelenika, Kristina; Vidaček, Renata; Ilijaš, Tomislav; Pavić, Petar (2017) - A significant porosity mismatch has been observed (especially for porosity values from 0 to 15%) when comparing core porosity data (corrected for overburden pressure and adjusted by depth) and the data obtained by petro- physical log analyses. In this way input porosity data are weighted according to prevailing lithofacies. Keywords: data; figure; kriging; methods; modelling; porosity; reservoirs; values
• Cluster defined sedimentary elements of deep-water clastic depositional systems and their 3D spatial visualization using parametrization: a case study from the Pannonian-basin by Horvath, Janina; Borka, Szabolcs; Geiger, János (2017) - Article history: Manuscript received January 31, 2017 Revised manuscript accepted April 24, 2017 Available online June 28, 2017 Keywords: cluster analysis, deep-water depositional system, geo-object, optimised clustering Figure 1. so this is a general problem as old as cluster analysis itself. Keywords: analysis; clustering; clusters; data; facies; lithofacies; method; number; study; variables
• 8th Croatian-Hungarian and 19th Hungarian geomathematical congress by Cvetković, Marko; Galović, Lidija (2017) - In general, handling geological data in the modern world is fairly difficult without a certain amount of mathe­ matical knowledge. Geomathematics covers a wide range of mathematical applica- tions in geosciences, ranging from simple data analysis to com- plex multivariate analysis, mapping algorithms, uncertainty ana­ lysis and neural networks. Keywords: data; geomathematical
• Heterogeneous hydraulic properties of an insular aquifer clarified by a tidal response method with simple decomposition techniques by Shirahata, Katsushi; Yoshimoto, Shuhei; Tsuchihara, Takeo; Ishida, Satoshi (2018) - doi: 10.6090/jarq.50.241 SHIRAHATA, K., YOSHIMOTO, S., TSUCHIHARA, T. & ISHIDA, S. (2017): Im- provements in a simple harmonic analysis of groundwater time series based on error analysis on simulated data of specified lengths.– The decomposition techniques and tidal response method em- ployed in the present study are explained below. Keywords: aquifer; data; fourier; groundwater; hydraulic; island; method; series; shirahata; site; time; time series
• Multi-point geostatistics for ore grade estimation by Song, Yu-Chen; Liu, Zhan-Ning; Meng, Hai-Dong; Yu, Xiao-Yan (2019) - A multi-point geostatistical simulation based on the reservoir skeleton (SMPS) used the shape, type, and scale of the target body Multi-point geostatistics for ore grade estimation Yu-Chen Song1, Zhan-Ning Liu1, Hai-Dong Meng1 and Xiao-Yan Yu1 1 Inner Mongolia University of Science and Technology, Institute of Mining Engineering, Baotou 014010, P.R. China; (songyuchen@imust.edu.cn; 494570031@qq.com; haidongm@imust.edu.cn; 421351047@qq.com) doi: 10.4154/gc.2019.23 Abstract A multi-point geostatistical method for ore grade estimation is introduced in order to fully utilize existing sampling information. This study proves the reliability and accuracy of the multi- point geostatistical method for ore grade estimation. Keywords: data; deviation; estimation; grade; grade estimation; image; li2o; li2o grade; method; model; number; ore; ore grade; point; ta2o5; ta2o5 grade; training; variogram
• Imputing missing data using grey system theory and the biplot method to forecast groundwater levels and yields by Ratković, Jelena; Polomčić, Dušan; Gligorić, Zoran; Bajić, Dragoljub (2022) - Upon reconstruction of the missing piezometric head data and total groundwater source yields, the gaps in the Bečej ground- water source (Bečej GS) data were filled over the study period. At groundwater sources, regular monitoring was hindered by poor organization and lack of instrumentation and human resources. Keywords: data; doi; grey; groundwater; method; model; observation; source; time; values