| 云南盈江邦朗寨铅锌矿成矿条件及找矿远景 |
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| 引用本文： | 冉启胜,黄兆熙,李良,朱淑桢.云南盈江邦朗寨铅锌矿成矿条件及找矿远景[J].云南地质,2014(4):561-565. |
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| 作者姓名： | 冉启胜 黄兆熙 李良 朱淑桢 |
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| 作者单位： | 云南省有色地质局308队,云南昆明650214 |
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| 摘 要： | 邦郎寨铅、锌多金属矿化体主要赋存于下元古界高黎贡山群下段（Pt1gl1）角闪片岩、板岩及硅质岩和结晶灰岩中,矿体由深部富含挥发分的含矿热液沿层间剥离滑脱构造充填成矿.并在断裂构造有利部位形成热液充填型铅、锌多金属隐伏矿体.
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| 关 键 词： | 层间滑脱构造 热液充填矿床 云南盈江邦朗寨 |
THE METALLOGENETIC CONDITIONS AND PROSPECTING POTENTIALITY OF BANGLANGZHAI PB-ZN DEPOSIT IN YINGJIANG,YUNNAN |
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| RAN Qi-sheng,HUANG Zhao-xi,LI Liang,ZHU Shu-zhen.THE METALLOGENETIC CONDITIONS AND PROSPECTING POTENTIALITY OF BANGLANGZHAI PB-ZN DEPOSIT IN YINGJIANG,YUNNAN[J].Yunnan Geology,2014(4):561-565. |
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| Authors: | RAN Qi-sheng HUANG Zhao-xi LI Liang ZHU Shu-zhen |
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| Institution: | (Geological Team 308, Yunnan Bureau of Nonferrous Geology, Kunming 650214) |
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| Abstract: | Banglangzhai Pb-Zn muhimetallic metallogenetic body is mainly in Lower Proterozoic Gaoligongs-han Group Lower Member （Pt1 gl1） hornblende schist, slate, siliceous rock and crystalline limestone. The ore- body is formed by the deep ore-bearing thermal fluid rich in volatile filling in the interlayer slide desquamation structure, and the hydrothermal filling type Pb-Zn multimetallic buried orebody is formed in the advantageous place of the fault structure. |
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| Keywords: | Interlayer Slide Desquamation Struture Hydrothermal Filling Ore Deposit Banglangzhai Yingjian Yunnan |
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