| 湘东北万古金矿的流体包裹体特征 |
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| 引用本文： | 安江华,李杰,陈必河,唐分配,谭仕敏,贺春平.湘东北万古金矿的流体包裹体特征[J].华南地质与矿产,2011,27(2):169-173. |
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| 作者姓名： | 安江华 李杰 陈必河 唐分配 谭仕敏 贺春平 |
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| 作者单位： | 湖南省地质调查院,长沙,410011 |
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| 基金项目： | 国土资源部南岭地区锡多金属矿调查评价项目，湖南省地质勘查开发局“湘东北地区与长江中下游斑岩型铜矿成矿地质条件对比及选区研究”项目 |
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| 摘 要： | 万古金矿位于位于平江县城西南.金矿（化）体产于中元古宙蓟县系变质岩中,严格受NWW向构造破碎带控制.金矿体呈似层状、透镜状.矿脉由含金石英脉和（或）含金破碎蚀带组成.流体包裹体研究表明,成矿流体温度较低(220～ 260℃),具有多源性,并以深源流体为主.
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| 关 键 词： | 流体包裹体 深源流体 金矿 万古 |
Fluid Inclusion Study of Wangu Gold Deposit, Northeastern Hunan Province |
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| AN Jiang-hua,LI Jie,CHEN Bi-he,TANG Fen-pei,TAN Shi-min,HE Chun-ping.Fluid Inclusion Study of Wangu Gold Deposit, Northeastern Hunan Province[J].Geology and Mineral Resources of South China,2011,27(2):169-173. |
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| Authors: | AN Jiang-hua LI Jie CHEN Bi-he TANG Fen-pei TAN Shi-min HE Chun-ping |
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| Institution: | (Hunan Institute of Geological Survey,Changsha 410011,China) |
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| Abstract: | Wangu gold deposit is located in the Pingjiang county,Hunan province.The mineralization was controlled by structural fracture zone,and emplaced in Middle Mesoproterozoic Jixianian System metamorphic rocks.The ore bodies are stratiform-like and lenticular composed of the gold-bearing quartz veins and cataclastic alteration zones.Fluid inclusion data of Wangu gold deposit show that the ore-forming fluid was characterized by low temperature(220 ~ 260℃).The ore-forming fluid was derived from various sources and mainly from the deep fluid. |
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| Keywords: | fluid inclusion deep fluid Wangu gold deposit northeastern Hunan province |
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