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首页> 外文期刊>Exploration and Mining Geology >The Orvan Brook Volcanogenic Massive Sulfide Deposit: Anatomy of a Highly Attenuated Massive Sulfide System, Bathurst Mining Camp, New Brunswick
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The Orvan Brook Volcanogenic Massive Sulfide Deposit: Anatomy of a Highly Attenuated Massive Sulfide System, Bathurst Mining Camp, New Brunswick

机译:Orvan Brook火山成块状硫化物矿床:新不伦瑞克省巴瑟斯特采矿营地高度衰减的块状硫化物系统的解剖

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摘要

The Orvan Brook deposit is one of several (Zn+PbCu)-rich sulfide deposits hosted by the Spruce Lake Formation (California Lake Group) in the northwestern part of the Bathurst Mining Camp. This parautochthonous deposit is hosted by a narrow band of highly deformed, locally graphitic shale that appears to conformably overlie felsic volcanic rocks of the Spruce Lake Formation, and is in tectonic contact with overlying mafic volcanic and related sedimentary rocks of the Canoe Landing Lake Formation.
机译:Orvan Brook矿床是位于美国西北部Spruce Lake组(加利福尼亚州Lake Group)拥有的几种富含(Zn + Pb Cu)的 硫化物矿床之一。 Bathurst采矿 营地。这种近地层沉积物由高度变形的局部石墨页岩的一条窄带 所容纳,看起来似乎 一致地覆盖了云杉湖 地层的长火山岩。 ,并且与上伏的镁铁质火山 以及独木舟登陆湖组的相关沉积岩形成构造接触。

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  • 来源
    《Exploration and Mining Geology 》 |2006年第4期| 155-176| 共22页
  • 作者单位

    New Brunswick Department of Natural Resources, Geological Surveys Branch, P.O. Box 50, Bathurst, New Brunswick, E2A 3Z1.;

    Department of Geology, University of New Brunswick, P.O. Box 4400, Fredericton, New Brunswick, E3B 5A3.;

    Department of Geology, University of New Brunswick, P.O. Box 4400, Fredericton, New Brunswick, E3B 5A3.;

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