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Uranium occurrences in the Cree Lake Zone, Saskatchewan, Canada

Published online by Cambridge University Press:  05 July 2018

G. R. Parslow
Affiliation:
Department of Geology, University of Regina, Regina, Saskatchewan S4S OA2
D. J. Thomas
Affiliation:
Department of Geology, University of Regina, Regina, Saskatchewan S4S OA2

Abstract

Over 100 samples of ‘pegmatite’ and associated host rocks from the Cree Lake Zone of northern Saskatchewan have been studied. The degree of U and Th enrichment of the pegmatites appears to depend on the parent material of the anatectic melts produced during the Hudsonian thermotectonic event. Evidence for Archaean granulite-facies depletion of U and Th is inconclusive; however, important enrichment of U and Th in the basal Aphebian is associated with metamorphosed black shales and possibly evaporates.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1982

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