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McArthur River Uranium Deposit. Saskatchewan, Canada

Farquharson, C.G. Craven, J.A. 2008. Three-dimensional inversion of magneto-telluric data for mineral exploration An example from the McArthur River uranium deposit, Saskatchewan, Canada. Journal of Applied Geophysics, in press. [Pg.443]

Vectoring potential of multi-element chemistry in unconformity-associated uranium deposits major and trace element signatures of the McArthur River Uranium Deposit, Saskatchewan, Canada. [Pg.493]

Derome, D., Cathehneau, M., Lhomme, T, Crmey, M. (2003). Fluid inclusion evidence of the differential migration of H2 and O2 in the McArthur River unconformity-type uranium deposit (Saskatchewan, Canada). Possible role on post-ore modifications of the host rocks. Journal of Geochemical Exploration, 7B-79, 525-530. [Pg.214]

Unconformity-type uranium deposits from the Athabasca Basin (Saskatchewan, Canada) represent the worid-richest uranium ores with the McArthur River deposit as a prime exampie. They are mainiy iocated ciose to the unconformity between a Paieo- to Meso-Proterozoic sedimentary basin, the Athabasca Basin, and an Archean to Paieoproterozoic metamorphic to piutonic basement. For severai years, a new type of uraniferous mineraiization, entireiy iocated in the basement, has been driiied in the South-Eastern part of the basin. Few data are avaiiabie for this type of deposit, iimiting the comparison of their characteristics and possibie genetic iinks with deposits iocated at the unconformity. [Pg.445]

Derome, D., Cathelineau, M., Cuney, M., Fabre, C., Lhomme, T., Banks, D.A. 2005. Mixing of sodic and calcic brines and uranium deposition at McArthur River, Saskatchewan, Canada. A raman and laser-induced breakdown spectroscopic study of fluid inclusions. Economic Geology, 100, 1529-1545. [Pg.459]

Canada and Australia are the world s largest producers of uranium. All Canadian production is from rich deposits in the Athabasca basin of northern Saskatchewan among those is the McArthur River mine, which has the world s largest high-grade deposit, estimated at 1.52 X 10 t of uranium from ore grading 15-18% uranium. These unconformity -type Saskatchewan deposits, which are also the principal deposit-type for Australian uranium production, contain mainly uraninite [UO2] with associated coffinite [U(Si04)i jc(0H)4j and brannerite [(U,Ca,Y,Ce)(Ti,Fe)206] (Plant et al, 1999). The chief uses of uranium are in nuclear power plants and weaponry. [Pg.4696]


See other pages where McArthur River Uranium Deposit. Saskatchewan, Canada is mentioned: [Pg.493]    [Pg.493]    [Pg.321]   


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