id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
geusb-8375	Ineson, Jon R; Peel, John S; Willman, Sebastian; Rugen, Elias J; Sønderholm, Martin; Frykman, Peter	Lithostratigraphy of the Portfjeld Group (Ediacaran – lowermost Cambrian) of North Greenland	2024	20	.pdf	application/pdf	9801	541	51	The base (see Slusen Formation) is a subpla- nar surface but irregular in detail with up to at least 5 metres of demonstrable relief where positive zones of fractured yet broadly in situ upper Slusen Formation dolostone rise above dolostone breccia with a sand- stone matrix. Caledonian orogenic belt Archaean Middle–Upper Proterozoic Fault Caledonian frontal thrusts Lower Palaeozoic Quaternary Lake / fjord River Cambro-Ordovician Buen Formation (lower Cambrian) Morænesø Formation (Neoproterozoic) Inuiteq Sø Formation (Palaeo–Mesoproterozoic) Portfjeld Group (Slusen Formation, Glaciologelv Formation) (Ediacaran/lowermost Cambrian) G.B. Schley Fjord Independence Fjord VGL KB J.C. Christensen Land Mylius-Erichsen Land C al ed on ia n fo re la nd an d pa ra ut oc ht ho n Peary Land Greenland ice sheet Wandel Dal Heilprin Land Greenland I Wulff Land NF FL a b 82°15´N Wandel Dal ØMSS NMSS Slusen Rundfjeld Chr.	cache/geusb-8375.pdf	txt/geusb-8375.txt