| 保山腊西山铜铅锌多金属矿地质特征 |
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| 引用本文： | 杨洪,胡成军,李泉,杨勇.保山腊西山铜铅锌多金属矿地质特征[J].云南地质,2011,30(2):144-147. |
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| 作者姓名： | 杨洪 胡成军 李泉 杨勇 |
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| 作者单位： | 云南省地质矿产勘查院大理地质矿产所,云南大理,671000 |
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| 摘 要： | 腊西山矿赋存在古生界崇山群变质岩系中,受区域性崇山西侧压扭性大断裂控制,矿(化)体分布于次级北西向断裂破碎带的矽卡岩碎裂岩内,矿化类型为矽卡岩型.
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| 关 键 词： | 矽卡岩型 铜铅锌多金属 断裂破碎带 崇山群川塘组 云南保山腊西山 |
THE GEOLOGY OF LAXISHAN CU- PB- ZN MULTIMETALLIC DEPOSIT, BAOSHAN |
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| YANG Hong,HU Cheng-jun,LI Quan,YANG Yong.THE GEOLOGY OF LAXISHAN CU- PB- ZN MULTIMETALLIC DEPOSIT, BAOSHAN[J].Yunnan Geology,2011,30(2):144-147. |
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| Authors: | YANG Hong HU Cheng-jun LI Quan YANG Yong |
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| Institution: | YANG Hong,HU Cheng-jun,LI Quan,YANG Yong(Dali Institute of Geology & Mineral Resources,Yunnan Exploration Institute of Geology & Mineral Resources,Dali 671000) |
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| Abstract: | The Laxishan ore deposit is in Palaeozoic Chongshan Group metamorphic rock series,which is controlled by the regional pressure-shear megafault west of Chongshan.And the ore body is in the skarn fracture rock in the NW secondary fault fracture zone.The metallogenesis belongs to the skarn type.. |
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| Keywords: | Skarn Type Cu-Pb-Zn Metallic Fault Fracture Zone Chongshan Group Chuantang Formation Laxishan Baoshan Yunnan |
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