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江西德兴朱砂红斑岩铜矿流体包裹体研究
引用本文:吴德新,赵元艺,吕立娜,许虹,郭硕,刘妍,朱小云,王增科,水新芳.江西德兴朱砂红斑岩铜矿流体包裹体研究[J].地质学报,2013,87(5):677-690.
作者姓名:吴德新  赵元艺  吕立娜  许虹  郭硕  刘妍  朱小云  王增科  水新芳
作者单位:中国地质大学(北京),中国地质科学院
摘    要:内容提要:朱砂红斑岩铜矿位于德兴斑岩铜矿矿集区的西北方向,紧邻铜厂铜矿。本文在前人有关德兴铜矿研究基础上,以铜矿流体包裹体为研究内容,通过野外详细的岩芯采样,室内石英斑晶、石英脉和方解石脉中包裹体测试及数据整理分析后初步发现:朱砂红斑岩铜矿流体包裹体大致可以分成五大类型(富液型包裹体、富气型包裹体、含CO2气液两相型包裹体、含子矿物多相型和固液两相型);相比铜厂整体成矿温度略低,盐度略高;由成矿流体压力47.27~184.47MPa,推导出成矿深度达2~4km,以及激光拉曼测试结果—流体中含有CO2、H2S和CH4等挥发分气体,它们可能与Au等元素的运移成矿有关。因此,从包裹体性质推测朱砂红铜矿不只是斑岩铜矿,可能是浅成热液斑岩型铜金矿床。此外,朱砂红矿区成矿流体来源至少有两种:高温岩浆流体和大气降水。伴随流体演化期次大致可以划分出三个成矿阶段:硅酸盐硫化物阶段、石英-硫化物阶段(即主成矿阶段,温度:200~340℃,盐度:2.0~15wt.%NaCl)、碳酸盐-硫酸盐硫化物阶段。同时,均一温度、盐度及压力等暗示在流体演化和成矿过程中岩浆流体发生过沸腾或不混溶作用。

关 键 词:德兴  朱砂红  斑岩铜矿  流体包裹体
收稿时间:4/2/2012 12:00:00 AM
修稿时间:2012/9/20 0:00:00

Study on fluid inclusions of Zhushahong porphyry copper deposit in Dexing, Jiangxi Province, and metallogenic dynamic significance
WU Dexin,ZHAO Yuanyi,Lv Lin,XU Hong,GUO Shuo,LIU Yan,ZHU Xiaoyun,WANG Zengke and SHUI Xinfang.Study on fluid inclusions of Zhushahong porphyry copper deposit in Dexing, Jiangxi Province, and metallogenic dynamic significance[J].Acta Geologica Sinica,2013,87(5):677-690.
Authors:WU Dexin  ZHAO Yuanyi  Lv Lin  XU Hong  GUO Shuo  LIU Yan  ZHU Xiaoyun  WANG Zengke and SHUI Xinfang
Institution:China University of Geosciences (Beijing), Beijing, 100083;MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, 100037;MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, 100037;China University of Geosciences (Beijing), Beijing, 100083;China University of Geosciences (Beijing), Beijing, 100083;MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, 100037;Jiangxi Copper Corporation Dexing Copper, Dexing, Jiangxi, 334200;Jiangxi Copper Corporation Dexing Copper, Dexing, Jiangxi, 334200;China University of Geosciences (Beijing), Beijing, 100083
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