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040 |aCaOODSP|beng|erda|cCaOODSP
043 |an-cn-ab|an-cn-sn
0861 |aM183-2/7462E-PDF
1001 |aAdlakha, Erin, |eauthor.
24510|aAlteration within the basement rocks associated with the P2 fault and the McArthur River uranium deposit, Athabasca Basin / |cE.E. Adlakha, K. Hattori, G. Zaluski, T. Kotzer and E.G. Potter.
264 1|a[Ottawa] : |bGeological Survey of Canada, |c2014.
264 4|c©2014
300 |a1 online resource (35 unnumbered pages) : |bcharts, illustrations, maps.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aOpen file ; |v7462
504 |aIncludes bibliographical references (pages [26-28]).
520 |a"The P2 reverse fault in the Athabasca Basin was a conduit for basinal fluids to enter the basement rocks below the regional unconformity and modify the rocks through fluid-rock interactions. Along the P2 fault, the basement rocks consist predominately of graphitic metapelite with quartzite and pegmatite. Immediately below the unconformity is an alteration profile consisting of a lower Green Zone with chlorite and illite, middle Red Zone dominated by hematite and kaolinite, and a discontinuous Bleached Zone of kaolin-group minerals and illite right at the unconformity. Preliminary data suggest that the alteration profile cannot be attributed solely to paleo-weathering but rather must include multiple fluid events from paleo-weathering through diagenetic to late hydrothermal fluids"--Abstract, page [3].
650 0|aBasins (Geology)|zAthabasca Basin (Sask. and Alta.)
650 6|aBassins (Géologie)|zAthabasca, Bassin d' (Sask. et Alb.)
651 0|aAthabasca Basin (Sask. and Alta.)
651 6|aAthabasca, Bassin d' (Sask. et Alb.)
7102 |aGeological Survey of Canada, |eissuing body.
830#0|aOpen file (Geological Survey of Canada)|v7462.|w(CaOODSP)9.832719
85640|qPDF|s8.90 MB|uhttps://publications.gc.ca/collections/collection_2025/rncan-nrcan/m183-2/M183-2-7462-eng.pdf
8564 |qHTML|sN/A|uhttps://doi.org/10.4095/293364