| 内蒙古道伦达坝铜多金属矿矿床地质特征及成因初探 |
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| 引用本文： | 李振祥,周福华,崔栋,李月新.内蒙古道伦达坝铜多金属矿矿床地质特征及成因初探[J].地质与资源,2009,18(1):27-30. |
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| 作者姓名： | 李振祥 周福华 崔栋 李月新 |
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| 作者单位： | 1. 内蒙古自治区第十地质勘查院, 内蒙古 赤峰 024005;2. 辽宁省地质矿产勘查院, 辽宁 沈阳 110032 |
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| 摘 要： | 道伦达坝铜多金属矿床主要产于北东向断裂带的构造裂隙中，矿体呈脉状，严格受断裂构造控制.矿床成因类型为充填交代型脉状矿床，属中高温热液矿床.该矿床处于大兴安岭中南部的锡林浩特-霍林郭勒多金属成矿带上，构造发育，岩浆活动频繁，铜多金属多期成矿.矿体规模为中小型，形态较复杂，厚度较稳定，组分较均匀到不均匀，围岩蚀变发育.
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| 关 键 词： | 铜多金属矿 矿床地质特征 控矿因素 矿床成因 道伦达坝 内蒙古 |
| 收稿时间： | 2008-09-23 |
GEOLOGY AND GENESIS OF THE DAOLUNDABA COPPER-POLYMETAL DEPOSIT IN INNER MONGOLIA |
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| LI Zhen-xiang,ZHUO Fu-hua,CUI Dong,LI Yue-xin.GEOLOGY AND GENESIS OF THE DAOLUNDABA COPPER-POLYMETAL DEPOSIT IN INNER MONGOLIA[J].Geology and Resources,2009,18(1):27-30. |
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| Authors: | LI Zhen-xiang ZHUO Fu-hua CUI Dong LI Yue-xin |
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| Institution: | 1. No. 10 Institute of Geological Exploration, Inner Mongolia Bureau of Geology and Mineral Resources, Chifeng 024005, Inner Mongolia, China;2. Liaoning Institute of Geological Exploration, Shenyang 110032, China |
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| Abstract: | The Daolundaba Cu-polymetal deposit in Xi Ujimqin Qi, Inner Mongolia, occurring in the structural fissures of NE-trending fault belt, is strictly controlled by the fault structure. The deposit is of filling-metasomatic vein type, genetically belonging to meso-hydrothermal deposit. The deposit is located in the Xilinhot-Huolin Gol polymetal metallogenetic belt in the middle-south of Daxinganling Mountains, with developed structure and frequent volcanic activities. The Cu-polymetallic mineralization is in mul... |
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| Keywords: | Cu-polymetal deposit geology of deposit ore-controlling factor genesis of deposit Inner Mongolia |
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