id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
gc-11	Vasiliev, Iuliana; Bakrač, Koraljka; Kovačić, Marijan; Abdoul Aziz, Hayfaa; Krijgsman, Wout	Palaeomagnetic Results from the Sarmatian/Pannonian Boundary in North-Eastern Croatia (Vranovi? Section, Našice Quarry)	2008	14	.pdf	application/pdf	6604	329	49	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).	cache/gc-11.pdf	txt/gc-11.txt