刘相利.赞比亚ICHIMPE铜钴矿矿床特征及成因[J].有色金属(矿山部分),2012,64(2):39-45.
赞比亚ICHIMPE铜钴矿矿床特征及成因
Mineralization characteristics and genesis of ICHIMPE Cu-Co Deposit in Zambia
投稿时间:2011-08-09  最后修改时间:2011-08-10
DOI:10.3969/j.issn.1671-4172.2012.02.012
中文关键词:  成因  矿床特征  铜钴矿
英文关键词:genesis  deposit characteristics  Cu-Co deposit
基金项目:
  
作者单位
刘相利 北京矿冶研究总院 北京 100070
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中文摘要:
      赞比亚ICHIMPE铜钴矿是赞比亚—刚果(金)铜矿带上的一个典型铜钴矿床,矿体赋存于下罗安组含矿建造中。在总结前人研究成果的基础上,简要论述了矿床的地质背景、含矿建造特征及矿床地质特征,并初步探讨了矿床成因及成矿规律,以期对本区的进一步探矿及评价起到促进作用。
英文摘要:
      The ICHIMPE Cu-Co Deposit is a typical deposit located in Zambia-Congo(DRC) Cu-Co metallogenic belt. Ore bodies occur in ore-bearing formations in the lower Roan Group. In order to promote further exploration and evaluation of this area, based on the summary of previous studies, this paper briefly describes the geological background, geological characteristics of ore-bearing formations and deposit, and discusses deposit genesis and metallogenic regularity.
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