id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
gc-243	Vlahović, Igor; Tišljar, Josip; Fuček, Ladislav; Oštrić, Nenad; Prtoljan, Božo; Velić, Ivo; Matičec, Dubravko	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)	2010	12	.pdf	application/pdf	5770	213	38	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.	cache/gc-243.pdf	txt/gc-243.txt