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The Millennium Uranium Deposit, Athabasca Basin, Saskatchewan, Canada: An Atypical Basement-Hosted Unconformity-Related Uranium Deposit

机译:加拿大萨斯喀彻温省阿萨巴斯卡盆地千年铀矿床:非典型地下室与不整合面有关的铀矿床

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摘要

The Millennium uranium basement-hosted unconformity-related deposit is one of the most recent discoveries of basement-hosted deposits, and may hold as much as 46.8 million pounds (18,000 metric tonnes U) at an average grade of 4.53 percent U3O8. The alteration zone associated with the deposit is atypical, as it consists predominantly of muscovite rather than the chlorite and muscovite commonly found in the other basement-hosted deposits of the Athabasca basin.
机译:千年铀基底托管的与不整合相关的 矿床是基底托管的 矿床的最新发现之一,可容纳多达4,680万磅(18,000 > 公吨U),平均品位为U 3 O 8 4.53%。与该矿床相关的 蚀变带是非典型的,因为 主要由白云母组成,而不是其他地下室中常见的绿泥石 和白云母-阿萨巴斯卡盆地的托管矿床

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  • 来源
    《Economic Geology》 |2009年第6期|815-840|共26页
  • 作者单位

    Department of Geological Sciences and Geological Engineering Queen’s University Kingston, Ontario, Canada K7L 3N6;

    Department of Geological Sciences and Geological Engineering Queen’s University Kingston, Ontario, Canada K7L 3N6;

    Department of Geological Sciences and Geological Engineering Queen’s University Kingston, Ontario, Canada K7L 3N6;

    Department of Geological Sciences and Geological Engineering Queen’s University Kingston, Ontario, Canada K7L 3N6;

    Cameco Corporation, 2121, 11th Street West, Saskatoon, Saskatchewan, Canada S7M 1J3;

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