缪远兴,郝玉军,董少波.刚果(金)卡莫亚铜钴矿床地质特征及成因探讨[J].矿产勘查,2014,5(2):350-355 |
刚果(金)卡莫亚铜钴矿床地质特征及成因探讨 |
Geological characteristics and genesis of Kamoya copper-cobalt deposit in Congo(DRC) |
投稿时间:2013-11-28 |
DOI: |
中文关键词: 铜钴矿床 刚果(金) 地质特征 矿床成因 找矿标志 |
英文关键词: copper-cobalt deposit D.R.Congo geological characteristics deposit genesis prospecting criteria |
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中文摘要: |
卡莫亚铜钴矿床位于中非赞比亚—刚果(金)铜钴成矿带内,与坎博韦大型铜钴矿床毗邻,为该成矿带上的典型矿床。矿床产于卡莫亚—坎博韦推覆体内,矿体赋存在中元古界加丹加群罗安组内。文章以卡莫亚铜钴矿床最新勘查资料为依据,对矿区地层、构造、矿体矿化特征等进行阐述,对矿床成因进行了探讨。卡莫亚铜钴矿床是受一定层位控制,经后期多次构造作用、热液叠加改造作用、变质热液叠加改造作用而形成的层控型铜钴矿床。根据野外找矿经验和综合研究分析,提出了该类矿床的找矿标志。 |
英文摘要: |
The Kamoya copper-cobalt deposit located in Zambia-D. R. Congo opper-cobalt metallogenic belt, is a typical copper deposit in this area near by the Kambove copper-cobalt deposit. The deposit occurs in the Kamoya-Kambovenappe structure,ore bodies occur in the Roan Group. This paper introduces the stratum, structure, ore body features, mineralization characteristics and discusses the deposit genesis based on the newly exploration information of Kamoya deposit.The deposit is a stratabound copper-cobalt deposit which occurs in a certain stratum, has experienced multi-phases of tectonic, hydrothermal superimposition and metamorphic hydrothermal superimposition. This paper proposes the prospecting criteria for this type of deposits in this area. |
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