| 云南武定刺竹箐铅锌矿矿床成因 |
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| 引用本文： | 庄荣寿.云南武定刺竹箐铅锌矿矿床成因[J].云南地质,2011,30(2):148-150. |
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| 作者姓名： | 庄荣寿 |
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| 作者单位： | 云南省有色地质局312队,云南安宁,650300 |
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| 摘 要： | 矿体赋存于主干断裂附近的次级构造裂隙中,分硫化矿和氧化矿,属热液充填型铅锌矿。
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| 关 键 词： | 构造裂隙铅锌矿 期后热液 浅表氧化矿 原生硫化物矿 云南武定刺竹箐 |
THE GENESIS OF CIZHUQING PB- ZN DEPOSIT IN WUDING, YUNNAN |
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| ZHUANG Rong-shou.THE GENESIS OF CIZHUQING PB- ZN DEPOSIT IN WUDING, YUNNAN[J].Yunnan Geology,2011,30(2):148-150. |
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| Authors: | ZHUANG Rong-shou |
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| Institution: | ZHUANG Rong-shou(Geological Team 312,Yunnan Bureau of Nonferrous Geology,Anning 650300) |
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| Abstract: | The ore body is in the secondary structural fissure near the principal fault,which belong to the Pb-Zn deposit of hydrothermal filling type and can be divided in to 2 types of sulfide and oxide |
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| Keywords: | Structural Fissure Type Postmagmatic Thermal Fluid Surface Oxidation Ore Original Sulfide Ore Cizhuqing Wuding Yunnan |
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