id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
gc-391		gc-391		2	.pdf	application/pdf	1673	82	78	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.	cache/gc-391.pdf	txt/gc-391.txt