id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
gc-466		gc-466		7	.pdf	application/pdf	2273	145	58	l. INTRODUCTION Several margin sequences of the Friuli Platform, representing the north western extension of the Dinaric Platform (Fig. l) during the latest Albian and Cenomanian, are characterized by pelagic influxes with planktonic organisms (COUSIN, 1981; GHETII, 1987; KOCH et al. , 1989; VENTURINI & TUNIS, 1990). Most of the grains of these carbonate sands are frag­ ments of fossils (Pl. l, l and 2 ; Pl.	cache/gc-466.pdf	txt/gc-466.txt