| 王如涛,朱谷昌,吴德文,石菲菲.赞比亚伊谦比铜钴矿床地质特征及成因研究[J].矿产勘查,2019,(9):2362-2372 |
| 赞比亚伊谦比铜钴矿床地质特征及成因研究 |
| Geological characteristics and genesis of Ichimpe copper-cobalt deposit in Zambia |
| 投稿时间：2019-08-24 |
| DOI： |
| 中文关键词: 尹谦比铜钴矿 地质特征 矿床成因 赞比亚 |
| 英文关键词: Ichimpe copper-cobalt deposit, geological characteristics genesis, Zambia |
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| 中文摘要: |
| 伊谦比(Ichimpe)铜钴矿产于非洲中南部赞比亚—刚果(金)铜钴成矿带上,邻近有谦比希、明多拉等大—中型铜钴矿床,本文在系统总结该矿床成矿地质背景、矿床地质特征的基础上,通过控矿因素和矿化富集规律两个方面,着重地分析了伊谦比(Ichimpe)铜钴矿床成因,认为矿床成因类型为沉积改造型铜钴矿床。 |
| 英文摘要: |
| Ichimpe copper-cobalt deposit is located in the Zambia-Congo(gold) copper-cobalt belt of central-southern Africa ,Which is near to the Chambishi and Mindola deposits. Based on the geological setting and Geological Characteristics of the Ichimpe Cu-Co deposit, It is analyzed the genesis briefly from the ore controlling factors and enrichment regularities of mineralization. The Ichimpe Copper-cobalt deposit should be the sedimentary-hydrothermal metasomatic deposit. |
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