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Geological setting of Precambrian supracrustal belts: a fundamental part of mineral resource evaluation in Greenland
Author(s) -
P.R Dawes,
H.K Schønwandt
Publication year - 1992
Publication title -
rapport
Language(s) - English
Resource type - Journals
eISSN - 2597-2944
pISSN - 0418-6559
DOI - 10.34194/rapggu.v155.8174
Subject(s) - precambrian , geology , proterozoic , mineral resource classification , geochemistry , shield , mineral , mineral exploration , earth science , paleontology , tectonics , materials science , metallurgy
In Precambrian shield areas the economic potential of supracrustal rocks is well documented, and some of the world's largest metal deposits are found within these sequences. The Black Angel lead-zinc stratabound mineralisation at Mårmorilik in central West Greenland (71° 10'N, Fig. 1), hosted in the Proterozoic Karrat Group, is one commercial enterprise that confirms that this potential can be realised in Greenland. In last year's volume of Report of Activities, Thomassen (1991a) gave a history of the geology and mineral exploration of the Black Angel deposit.

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