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001	9.956859
003	CaOODSP
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008	251029t20142014oncdab  ob   f|0| 0 eng d
040	|aCaOODSP|beng|erda|cCaOODSP
043	|an-cn-sn|an-cn-ab
086	1 |aM183-2/7463E-PDF
100	1 |aDann, J., |eauthor.
245	10|aDiscrimination of elemental assemblages in the alteration halo of the Phoenix deposit, Saskatchewan, through applied GIS / |cJ. Dann, K. Hattori, E.G. Potter and C. Sorba.
264	1|a[Ottawa] : |bGeological Survey of Canada, |c2014.
264	4|c©2014
300	|a1 online resource (66 unnumbered pages) : |bcharts, illustrations, maps.
336	|atext|btxt|2rdacontent
337	|acomputer|bc|2rdamedia
338	|aonline resource|bcr|2rdacarrier
490	1 |aOpen file, |x2816-7155 ; |v7463
504	|aIncludes bibliographical references (pages [65-66].
520	|a"This study was initiated as part of the TGI-4 uranium ore systems project to evaluate the dispersion of ore-related elements that could be used to increase exploration effectiveness for deeply buried, unconformity-related uranium mineralization. The Phoenix deposit, located in the Athabasca Basin, currently has indicated resources of approximately 52.3 million lbs U3O8. The mineralization consists of four pods termed the A, B, C and D ore zones at ca. 400 meters depth. The pods occur both at the unconformity and within the basement as steeply dipping zones associated with a fault zone termed the WS shear"--Abstract, page [3].
650	0|aUranium ores|xGeology|zAthabasca Basin (Sask. and Alta.)
650	6|aUranium|xGisements|xGéologie|zAthabasca, Bassin d' (Sask. et Alb.)
710	2 |aGeological Survey of Canada, |eissuing body.
830	#0|aOpen file (Geological Survey of Canada)|v7463.|w(CaOODSP)9.506878
856	40|qPDF|s11.00 MB|uhttps://publications.gc.ca/collections/collection_2025/rncan-nrcan/m183-2/M183-2-7463-eng.pdf
856	4 |qHTML|sN/A|uhttps://doi.org/10.4095/293122