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;
机译:江西南部Maoping Tungsten矿床流体演化与垂直区划的联系:流体包容性和稳定同位素证据
机译:回答Marignac和Cathelineau在Sánchez-España等人的论文中的评论:伊比利亚黄铁矿带北部大块硫化物矿床中成矿热液的来源和演化:来自流体包裹体和稳定同位素的证据(矿物矿床38:519–537)
机译:Sanchez-España等人对该论文的评论:伊比利亚北部黄铁矿带大量硫化物矿床中成矿热液的来源和演化(西班牙西南):流体包裹体和稳定同位素的证据(矿物矿床38:519–537) )
机译:云南东北昭通造黄油锌矿床成矿液的演变:血管宿主流体夹杂物的证据
机译:入侵过程中哈里森山口岩体周围流体循环的场,流体包裹体和同位素化学证据:卡林型沉积物的流体模型。
机译:锌/镉比和镉同位素证明铅锌矿床的分类
机译:磁铁矿中成矿液中的矿石液的起源和演变岩石矿床(BAFQ):流体夹杂物和氧气稳定同位素的证据