| 王鹏飞.刚果(金)MKM铜钴矿床地质特征[J].矿产勘查,2018,9(10):2007-2014 |
| 刚果(金)MKM铜钴矿床地质特征 |
| Geological Features of Myunga-Kalumbwe Copper-CobaltMine of DR Congo |
| 投稿时间：2018-05-17 |
| DOI： |
| 中文关键词: 刚果(金) 铜钴矿床特征 加丹加岩系 推覆构造 |
| 英文关键词: DR Congo,characteristics of copper-cobalt deposit, Katanga series, nappe structure |
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| 中文摘要: |
| MYUNGA-KALUMBWE(以下简称MKM)铜钴矿区位于世界第三大铜矿带--南非赞比亚-刚果(金)矿带的北西部,是一个具有百年开采历史的老矿区。MKM矿床为大型层控型矿床,主矿体位于倒转背斜轴部,受区域浅变质作用和后期改造而富集。矿体主要赋存于加丹加岩系罗安群内一套受了区域变质作用的陆源碎屑岩和白云岩地层中。通过对区域成矿地质背景和MKM矿床地质特征的分析,总结了控矿地质因素、矿床成因类型等。 |
| 英文摘要: |
| Myunga-Kalumbwe copper-cobalt mine is located on the northwest area of the South Africa-Zambia-DR Congo copper belt, which is the third largest copper mine belt of the world. It has been explored over one hundred years. Myunga-Kalumbwe copper-cobalt deposit is the large-scale stratiform deposit. The main ore body is located on the axis of converted anticline, which is controlled by regional shallow metamorphism and post-alteration concentration. Based on the analysis of regional metallogenic geological background and geological characteristics of MKM deposit, the ore controlling geological factors and genetic types of ore deposits are summarized in this paper. |
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