Acritarchs from the Proterozoic Thule Group, North-West Greenland

G Vidal, P.R Dawes
1980 Rapport Grønlands Geologiske Undersøgelse  
A thick sequence of Proterozoic sedimentary and volcanic rocks (the Thule Group), penetrated in part by basic minor intrusions, characterises the Thule district of North-West Greenland (fig. 6). These strata, overlying the Greenland Shield with profound unconformity, form a large intracratonic basin on Ihe northern margin af the North American Greenland craton (Dawes, 1976).
doi:10.34194/rapggu.v100.7689 fatcat:y6ey6bhn4vgt7cm6pi7534t2ga