id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
gc-468		gc-468		20	.pdf	application/pdf	11581	908	60	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.	cache/gc-468.pdf	txt/gc-468.txt