| Reference Type | Journal (article/letter/editorial) |
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| Title | Uranium occurrences in the Cree Lake Zone, Saskatchewan, Canada |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Parslow, G. R. | Author |
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| Thomas, D. J. | Author |
| Year | 1982 (June) | Volume | 46 |
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| Issue | 339 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_46/46-339-163.pdf+ |
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| DOI | doi:10.1180/minmag.1982.046.339.02Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3380 | Long-form Identifier | mindat:1:5:3380:4 |
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| GUID | 0 |
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| Full Reference | Parslow, G. R., Thomas, D. J. (1982) Uranium occurrences in the Cree Lake Zone, Saskatchewan, Canada. Mineralogical Magazine, 46 (339) 163-171 doi:10.1180/minmag.1982.046.339.02 |
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| Plain Text | Parslow, G. R., Thomas, D. J. (1982) Uranium occurrences in the Cree Lake Zone, Saskatchewan, Canada. Mineralogical Magazine, 46 (339) 163-171 doi:10.1180/minmag.1982.046.339.02 |
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| In | (1982, June) Mineralogical Magazine Vol. 46 (339) Mineralogical Society |
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| Abstract/Notes | AbstractOver 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. |
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