| 云南泸水自把铅矿矿床地质及成因 |
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| 引用本文： | 肖祥春,陶云花.云南泸水自把铅矿矿床地质及成因[J].云南地质,2012(2):200-203,199. |
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| 作者姓名： | 肖祥春 陶云花 |
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| 作者单位： | 云南黄金矿业集团股份有限公司 |
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| 摘 要： | 矿床受地层及断层双重控制,走向长大于3千米,共圈出V1、V2、V3三条矿体。含矿岩石以透辉石矽卡岩为主,矿石工业类型为硫化铅矿石和氧化铅矿石。矿床成因类型为与花岗岩有关的含矿热液沿破碎带充填-交代形成的矽卡岩型铅矿床。
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| 关 键 词： | 矽卡岩型铅矿 热液充填交伏 断层破碎带 与花岗岩有关 云南泸水自把 |
THE GEOLOGY AND GENESIS OF ZIBA PB DEPOSIT OF LUSHUI,YUNNAN |
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| XIAO Xiang-chun,TAO Yun-hua.THE GEOLOGY AND GENESIS OF ZIBA PB DEPOSIT OF LUSHUI,YUNNAN[J].Yunnan Geology,2012(2):200-203,199. |
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| Authors: | XIAO Xiang-chun TAO Yun-hua |
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| Institution: | (Yunnan Company(Ltd)of Au Mining Industry(Group),Kunming 650215) |
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| Abstract: | The ore deposit is controlled by the bed and fault,strike NW,dip NE,length more than 3000m.There are 3 ore bodies,V1,V2,V3.The main ore-bearing rock is the dioside skarn.The commercial ores are Pb sulfide and Pb oxide.It belongs to the Pb deposit of skarn type,which is formed by the filling and metasomatism of thermal fluid related with the granite. |
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| Keywords: | Skarn Pb Deposit Filling and metasomatism of Thermal Fluid Fault Fracture Zone Related with Granite Ziba Lushui Yunnan |
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