id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
gc-433		gc-433		11	.pdf	application/pdf	5901	284	54	\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)	cache/gc-433.pdf	txt/gc-433.txt