首页> 外文会议>Quadrennial International Association on the Genesis of Ore Deposits Symposium;Geological Society of China >The Evolution of Ore-forming Fluid of Maoping Lead-Zinc Deposit, Zhaotong in Northeast Yunnan: the Evidence of Sphalerite-hosted Fluid Inclusions
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The Evolution of Ore-forming Fluid of Maoping Lead-Zinc Deposit, Zhaotong in Northeast Yunnan: the Evidence of Sphalerite-hosted Fluid Inclusions

机译:滇东北昭通茅坪铅锌矿床成矿流体演化:闪锌矿型流体包裹体的证据

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  • 会议地点 Kunming(CN)
  • 作者单位

    Faculty of Land Resources and Engineering, Southwest Institute of Geological Survey, Geological Survey Center forNon-ferrous Mineral Resources, Kunming University of Science and Technology, Kunming 650093, China E-mail: qiuwenlong2005@126.com;

    Faculty of Land Resources and Engineering, Southwest Institute of Geological Survey, Geological Survey Center forNon-ferrous Mineral Resources, Kunming University of Science and Technology, Kunming 650093, China;

    State Key Laboratory for Mineral Deposit Research, Institute of Geo-Fluid, School of Earth Science and Engineering,Nanjing University, Nanjing 210093, China;

    Yunnan Copper Industry (Group) Co., Ltd, Kunming prospecting Design Institute of China Nonferrous Metals Industry,Kunming 650051, China;

    Faculty of Land Resources and Engineering, Southwest Institute of Geological Survey, Geological Survey Center forNon-ferrous Mineral Resources, Kunming University of Science and Technology, Kunming 650093, China;

    Faculty of Land Resources and Engineering, Southwest Institute of Geological Survey, Geological Survey Center forNon-ferrous Mineral Resources, Kunming University of Science and Technology, Kunming 650093, China;

    State Key Laboratory for Mineral Deposit Research, Institute of Geo-Fluid, School of Earth Science and Engineering,Nanjing University, Nanjing 210093, China;

    State Key Laboratory for Mineral Deposit Research, Institute of Geo-Fluid, School of Earth Science and Engineering,Nanjing University, Nanjing 210093, China;

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