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TitleThe paragenesis and chemistry of alteration associated with the P2 fault in metamorphic rocks underlying the Athabasca Basin
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AuthorAdlakha, E E; Hattori, K; Potter, E G; Sopuck, V
SourceGeological Survey of Canada, Open File 7365, 2013, 1 sheet, https://doi.org/10.4095/292559 (Open Access)
Image
Year2013
PublisherNatural Resources Canada
Meeting2013 PDAC-SEG Canadian Student Chapter Mineral Colloquium; Toronto; CA; March 3-5, 2013
Documentopen file
Lang.English
Mediaon-line; digital
File formatpdf
ProvinceSaskatchewan
NTS74H
AreaKey Lake; McArthur River
Lat/Long WENS-106.0000 -104.0000 58.0000 57.0000
Subjectsmineralogy; economic geology; geochemistry; geochemical anomalies; uranium; uranium deposits; mineralization; mineral deposits; geochemical analyses; sedimentary rocks; sandstones; unconformities; unconformity-type deposit; paragenesis; alteration; Athabasca Basin; Phoenix Deposit; P2 Fault; Precambrian
Illustrationslocation maps; photographs; plots; cross-sections
ProgramUranium Ore Systems, Targeted Geoscience Initiative (TGI-4)
Released2013 05 02
Summary(Plain Language Summary, not published)
Currently, all of Canada's uranium production comes from the Athabasca Basin. The McArthur River and nearby Millennium deposits are spatially associated with a regional fault system termed the P2 structure. At McArthur River, high-grade mineralization is bound by the regional P2 and the local VQ fault systems. The spatial relationship implies that the structures played a role in focusing ore-forming fluids during creation of the deposit. This study aims to build on that hypothesis by documenting subtle mineralogical, geochemical and isotopic changes in the fault systems as they approach the deposit.
GEOSCAN ID292559