id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
geusb-4818	Thrane, Kristine	Palaeoproterozoic age of a basement gneiss complex in the Charcot Land tectonic window, East Greenland Caledonides	2004	10	.pdf	application/pdf	6208	275	62	The Charcot Land window (Fig. 2) exposes a base- ment complex of grey gneisses with amphibolite bands, overlain by a cover of low to medium-grade supracrustal rocks including carbonates, volcanic rocks and siliciclastic sediments (Charcot Land supracrustal sequence; Steck 1971). The crystalline gneisses making up the Flyver- fjord infracrustal complex in Hinks Land, south-east of Charcot Land (Fig. 2), are of late Archaean age (c. 2700 Ma; Rex & Gledhill 1974; Thrane 2002).	cache/geusb-4818.pdf	txt/geusb-4818.txt