| 内蒙古克什克腾旗双山子银铅锌矿地质特征及成因 |
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| 引用本文： | 赵金才,闫志强,迟永坤,周文光,董存杰,杨淑红.内蒙古克什克腾旗双山子银铅锌矿地质特征及成因[J].地质与资源,2010,19(2):134-137,150. |
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| 作者姓名： | 赵金才 闫志强 迟永坤 周文光 董存杰 杨淑红 |
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| 作者单位： | 辽宁省有色地质局108队, 辽宁 沈阳 110013 |
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| 摘 要： | 双山子区位于乌兰浩特-巴林右旗铜多金属成矿带的南西端，目前共发现有5条银铅锌盲矿体.区内银铅锌矿体主要受早期北东东向断裂构造所控制，铅锌矿（化）体具有集中分布于火山碎屑角砾岩内及其边部的特征，矿床属于岩浆热液型矿床成因.区内呈北东东向以不规则状出现的物探激电异常、中低视电阻率异常与△T磁异常及较高浓度Ag、Cu、Pb、Zn、As等元素的土壤异常分布区，是本区重要的找矿信息和标志.
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| 关 键 词： | 内蒙古 双山子 银铅锌矿床 岩浆热液型矿 物化探异常 找矿标志 |
| 收稿时间： | 2010-05-11 |
GEOLOGY AND GENESIS OF THE SHUANGSANZI Ag-Pb-Zn DEPOSIT IN INNER MONGOLIA |
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| ZHAO Jin-cai,YAN Zhi-qiang,CHI Yong-kun,ZHOU Wen-guang,DONG Cun-jie,YANG Shu-hong.GEOLOGY AND GENESIS OF THE SHUANGSANZI Ag-Pb-Zn DEPOSIT IN INNER MONGOLIA[J].Geology and Resources,2010,19(2):134-137,150. |
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| Authors: | ZHAO Jin-cai YAN Zhi-qiang CHI Yong-kun ZHOU Wen-guang DONG Cun-jie YANG Shu-hong |
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| Institution: | No. 108 Geologic Party, Liaoning Bureau of Nonferrous Metal Geology, Shenyang 310013, China |
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| Abstract: | The Shuangsanzi area is located in the southwest end of the Ulanhot-Balinyouqi Cu-polymetal metallogenic belt,where five Ag-Pb-Zn blind orebodies have been found.The orebodies are mainly controlled by the early NEE-trending faults and intensively distributed in and around the pyroclastic breccia.The deposits genetically belong to magmatic hydrothermal type.They occur in a zone of NEE direction,with irregular-shaped geophysical anomaly and rich Ag,Cu,Pb,Zn and As soil anomaly.All of those are important prospecting information and indicators in the area. |
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| Keywords: | Inner Mongolia Shuangsanzi Ag-Pb-Zn deposit magmatic hydrothermal type geophysical and geochemical exploration indicator |
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