| 内蒙古太仆寺旗金豆子山铅锌矿床地质特征及成因探讨 |
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| 引用本文： | 陈建国.内蒙古太仆寺旗金豆子山铅锌矿床地质特征及成因探讨[J].甘肃冶金,2011,33(2):89-91,103. |
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| 作者姓名： | 陈建国 |
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| 作者单位： | 甘肃有色地质勘查局三队,甘肃,白银,730900 |
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| 摘 要： | 矿床位于华北地台北缘、白云鄂博裂谷带中,赋存于中元古界白云鄂博群地层中,属中低温热液矿床,受断裂破碎带控制.本文通过对矿床区域成矿地质背景、矿区及矿体地质特征研究,探讨了矿床成因及控矿因素.
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| 关 键 词： | 内蒙古太仆寺旗 金豆子山铅锌矿 地质特征 成因 |
Discussion on Geological Characteristics and Genesis of the Jindouzishan Lead-zinc Deposit of Taipusi Banner in the Inner Mongolia |
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| CHEN Jian-guo.Discussion on Geological Characteristics and Genesis of the Jindouzishan Lead-zinc Deposit of Taipusi Banner in the Inner Mongolia[J].Gansu Metallurgy,2011,33(2):89-91,103. |
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| Authors: | CHEN Jian-guo |
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| Affiliation: | CHEN Jian-guo(The Third Team of Gansu Non-ferrous Metal Geological Exploration Bureau,Baiyin 730900,China) |
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| Abstract: | The deposit is located in the northern margin of the North China Platform and Bayunebo rift belt,hosted in Proterozoic strata of the Bayunebo Group,which is in the low-temperature hydrothermal deposit,controlled by the fractured zone.Based on the deposits in the regional geological setting,mining and geological characteristics of ore body,explores the genesis and ore-controlling factors. |
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| Keywords: | Taipusi Banner in the Inner Mongolia Jindouzishan lead-zinc deposit geological characteristics genesis |
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