| 智利MARCIA铜矿地质特征及成矿机理 |
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| 引用本文： | 李忠烈.智利MARCIA铜矿地质特征及成矿机理[J].矿产与地质,2012,26(3):228-230. |
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| 作者姓名： | 李忠烈 |
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| 作者单位： | 河南省有色金属地质勘查总院 |
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| 摘 要： | MARCIA铜矿位于智利海岸山脉成矿带,通过对矿区地层、地质特征、矿体特征与构造的关系等分析,对该矿区铜矿的形成机理进行了初步探讨,认为该矿区铜矿的形成与断裂关系密切,F2断裂是导矿和容矿断裂,该区找矿前景巨大.
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| 关 键 词： | 铜矿床 地质特征 成矿机理 智利 |
Geological characteristics and metallogenic mechanism of the Marcia copper deposit in Chile |
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| LI Zhong-lie.Geological characteristics and metallogenic mechanism of the Marcia copper deposit in Chile[J].Mineral Resources and Geology,2012,26(3):228-230. |
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| Authors: | LI Zhong-lie |
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| Institution: | LI Zhong-lie(Henan Institute of Non-ferrous Metals Geological Exploration,Zhengzhou 450052) |
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| Abstract: | The Marcia copper deposit is located in IOCG belt.Through analyzing the strata,geological characteristics,the orebody characteristics and tectonic features of the mining area,the metallogenic mechanism of the copper deposit was discussed.It has concluded that the formation of copper deposit in the mine are closely to the fault,the F2 fault is ore-transmitting and ore-containing fault and it has great prospecting potential in this area. |
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| Keywords: | Chile copper geological characteristics metallogenic mechanism |
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