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Please use this identifier to cite or link to this item: http://hdl.handle.net/1993/3983

Title: The geology and geochemistry of the Millennium uranium deposit, Athabasca basin, Saskatchewan, Canada
Authors: Beshears, Charles J.
Supervisor: Fayek, Mostafa (Geological Sciences)
Examining Committee: Camacho, Alfredo (Geological Sciences) Jiricka, Dan (Cameco Inc.)
Graduation Date: May 2010
Keywords: uranium
geochemistry
isotopes
geology
Issue Date: 19-Apr-2010
Abstract: The Millennium uranium deposit is located 35 km north of the Key Lake mine, Saskatchewan. Uranium mineralization occurs in a variety of styles including (1) massive replacement, (2) fracture filling veins, (3) fine-grain aggregates associated with “mini” roll fronts, and (4) disseminated grains. The chemical Pb and isotopic 207Pb/206Pb ages of the massive (style 1), vein-type (style 2), and fine-aggregate (style 3) uraninite cluster at 1400-1200 and 1100-900 Ma. The ~1400 Ma ages coincide with the primary mineralization event for many of the uranium deposits (1550-1400 Ma) within the Athabasca Basin. Unlike other uranium deposits from the Athabasca basin, disseminated uraninite (style 4) have 207Pb/206Pb ages from 1770-1650 Ma. These ages are older than the depositional age for the Athabasca sediments (~1710 Ma) and are similar to the ages from the Beaverlodge vein-type uranium deposits.
URI: http://hdl.handle.net/1993/3983
Appears in Collection(s):FGS - Electronic Theses & Dissertations (Public)

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