The Aeromag 2001 survey covers a part of central West Greenland between Uummannaq and Prøven and includes both onshore and offshore areas. The survey will provide valuable information for the exploration of both mineral and hydrocarbon resources.
The area between Uummannaq and Prøven is characterised by an Archaean crystalline basement, an impressive succession of Palaeoproterozoic sediments intruded by a granitic complex, minor outcrops of down faulted Cretaceous sediments, and Tertiary plateau basalts. The Archaean rocks, which have been correlated with similar rocks on neighbouring Baffin Island in Canada, were folded and metamorphosed during the Hudsonian orogeny c. 1.85 Ga and intruded by a 1.65 Ga old dolerite dyke swarm.
The Palaeoproterozoic Karrat Group hosts the now exhausted Black Angel lead-zinc deposit which was mined 1973–1990. Similar marble-hosted lead-zinc occurrences at other localities indicate an additional potential for this type of mineralisation. The clastic rocks of the Karrat Group comprise extensive sulphide facies iron-formation and vein-type mineralisation with base and precious metals. Additionally, the group offers a potential for shale-hosted sulphides and turbedite-gold-bearing veins and shear zones. The Tertiary volcanic rocks have units of extremely reduced lavas with native iron, indicating a potential for Ni-Cu-PGM Norilsk-type occurrences.
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