Uranium Geology And Geochemistry Copper Mountain , Wyoming

Society for Mining, Metallurgy & Exploration
L. B. Bramlett
Organization:
Society for Mining, Metallurgy & Exploration
Pages:
23
File Size:
2363 KB
Publication Date:
Jan 1, 1980

Abstract

The Archean (2.65 b.y.) aged Canning Stock at Copper Mountain, Wyoming contains an average of 20 ppm U. The North Canning and Fuller deposits occur within the enriched interior of the stock. Post-Laramide development of super gene enrichment blankets occurred in wide (25- 100 m) crushed zones. Hematite and chlorite accompany pyrite and sooty pitchblende in the mineralized zones. Reduction mechanisms proposed for deposition of pitchblende are: 1) sulfides, 2) hydrocarbons, 3) bacteria, 4) the water table, or 5) some combination of these. Abundant tar- type organics appear to have preserved the enrichment blankets from degradation. Trace element and radiometric data define target zones, but exploration models focus on favorable structure.
Citation

APA: L. B. Bramlett  (1980)  Uranium Geology And Geochemistry Copper Mountain , Wyoming

MLA: L. B. Bramlett Uranium Geology And Geochemistry Copper Mountain , Wyoming. Society for Mining, Metallurgy & Exploration, 1980.

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