| 云南镇沅蝙蝠山金矿成因探讨 |
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| 引用本文： | 范建辉,赵含军,张志平.云南镇沅蝙蝠山金矿成因探讨[J].云南地质,2012(2):159-162. |
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| 作者姓名： | 范建辉 赵含军 张志平 |
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| 作者单位： | 云南省地质矿产局普洱管理处 |
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| 摘 要： | 蝙蝠山金矿属超基性岩接触带型。金矿受地层、构造、基性岩的控制。由多期成矿作用、多源物质来源、多成因成矿热液,反复活化、迁移、聚集、分配和积淀形成。
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| 关 键 词： | 混合中温热液 变质侧分泌 黄铁矿白云石型 韧性剪切带 云南镇沅蝙蝠山 |
A PROBE INTO THE GENESIS OF BIANFUSHAN AU DEPOSIT OF ZHENYUAN,YUNNAN |
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| FAN Jian-hui,ZHAO Han-jun,ZHANG Zhi-ping.A PROBE INTO THE GENESIS OF BIANFUSHAN AU DEPOSIT OF ZHENYUAN,YUNNAN[J].Yunnan Geology,2012(2):159-162. |
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| Authors: | FAN Jian-hui ZHAO Han-jun ZHANG Zhi-ping |
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| Institution: | (Simao Administration of Yunnan Bureau of Geology & Mineral Resources,Simao 665000) |
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| Abstract: | The Bianfushan Au deposit belongs to the Au metallogenesis zone of ultrabasic rock contact.It is controlled by sedimentary rock bed,structure and basic igneous rock.The Au deposit is formed by the repeat activization,migration,aggregation,distribution and precipitation of multiperiodic metallogenesis,polygenetic sources and metallogenetic thermal fluid. |
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| Keywords: | Mixed Middle T Thermal Fluid Metamorphic Lateral Secretion Pyrite-Dolomite Type Ductile Shear Zone Bianfushan Au Deposit |
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