| 内蒙古自治区阿尔哈达铅锌矿矿床地质特征 |
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| 引用本文： | 陶则熙.内蒙古自治区阿尔哈达铅锌矿矿床地质特征[J].地质找矿论丛,2006,21(Z1):74-76. |
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| 作者姓名： | 陶则熙 |
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| 作者单位： | 中国冶金地质勘查工程总局,第一地质勘查院,河北,三河,065201 |
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| 摘 要： | 阿尔哈达铅锌矿产于中酸性岩体附近的泥盆系、二叠系中,受与NE向断裂贯通的成群(组)出现的次级断裂控制;矿体连续性较好,平面上呈透镜状,空间上呈柱状、似板状、透镜状,矿体为隐伏-半隐伏状,埋深不大;矿床属于中低温热液矿床.
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| 关 键 词： | 阿尔哈达铅锌矿 矿床地质特征 内蒙古自治区 |
| 文章编号： | 1001-1412(2006)S0-0074-03 |
| 修稿时间： | 2006年7月4日 |
GEOLOGICAL CHARACTERISTICS OF ARHADA LEAD & ZINC DEPOSIT IN DONGWUQI COUNTY,INNER MONGOLIA, CHINA |
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| TAO Ze-xi.GEOLOGICAL CHARACTERISTICS OF ARHADA LEAD & ZINC DEPOSIT IN DONGWUQI COUNTY,INNER MONGOLIA, CHINA[J].Contributions to Geology and Mineral Resources Research,2006,21(Z1):74-76. |
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| Authors: | TAO Ze-xi |
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| Abstract: | Arhada Pb-Zn deposit is located in strata of Devonian and Permian System near intermediate-acidic intrusive rocks and controlled by the NE fault-traversed sub-scale faults.Ore bodies are continuous and look lenses in plan and spatially look pillars,tabulate bodies,lenses.They are semi-buried-buried.The deposit is a mesothermal-low temperature deposit. |
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| Keywords: | Arhada Pb-Zn deposit geological characteristics Inner Mongolia |
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