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Acritarchs from the Proterozoic Thule Group, North-West Greenland
Author(s) -
Gonzalo Vidal,
P.R Dawes
Publication year - 1980
Publication title -
rapport
Language(s) - English
Resource type - Journals
eISSN - 2597-2944
pISSN - 0418-6559
DOI - 10.34194/rapggu.v100.7689
Subject(s) - geology , proterozoic , unconformity , craton , acritarch , paleontology , group (periodic table) , structural basin , shield , sequence (biology) , volcano , tectonics , chemistry , genetics , organic chemistry , biology
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).

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