id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
geusb-4692	Upton, Brian G J	Tectono-magmatic evolution of the younger Gardar southern rift, South Greenland	2013	128	.pdf	application/pdf	67653	3522	58	Apparently homogeneous gabbros form 200 m thick marginal border groups that grade, through a few metres of iron-rich syenogabbro, into a vertical zone several metres broad, displaying a spectacular ar- ray of directionally oriented, branching, clinopyroxene N 250 140 240 230 110 170 115 170 Arfersuaq Asorutit Nasaasarli 305 Krydssø Sigssarluttoq Troctolitic gabbro Krydssø syenogabbro Assorutit quartz syenite Younger Gardar dyke complex Older Gardar dyke complex Foyaites Julianehåb batholith Section a–a’ Section b–b’ Kryd ssø 1 km b b’ a a’ A B 46°15´ 61° 60°54´ Fig. 17 (Modified from Upton 1962, 1964a). Younger giant dyke complex Tugtutôq central complex Older giant dyke complex Julianehåb batholith Fault Fault A B Tuttu tooq Sto r e Pil esø Sejlfjord 45°30´ 60°51´ 17 reaction fringes and fluor-apatite are minor components.	cache/geusb-4692.pdf	txt/geusb-4692.txt