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Summary of studying on metallogenesis of magmatic Ni-Cu-PGE sulfide deposits

机译:岩浆Ni-Cu-PGE硫化物矿床成矿研究综述

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1 IntroductionAs the typical deposit of magmatic segregation, Magmatic Ni-Cu±platinum-group element (PGE) sulfide deposits are important deposit type. Its exploitation amounts on Cu,PGE is more than half of the world total, it is also the main copper industry type especially in China. The studies on magmatic sulfide deposits had began eighty years ago, and have gotten some important study results(Wang et al., 2003). This paper summarized simply the metallogenesis of magmatic Ni-Cu-PGE sulfide deposits, hoping to contribute the exploration and studying on Chinese magmatic Ni-Cu-PGE sulfide deposits.
机译:1引言作为典型的岩浆偏析矿床,岩浆Ni-Cu±铂族元素(PGE)硫化物矿床是重要的矿床类型。它在铜,铂族金属上的开采量占世界总量的一半以上,也是主要的铜工业类型,尤其是在中国。岩浆硫化物矿床的研究始于八十年前,并取得了重要的研究成果(Wang等,2003)。本文简单总结了岩浆Ni-Cu-PGE硫化物矿床的成矿作用,以期为我国岩浆Ni-Cu-PGE硫化物矿床的探索与研究做出贡献。

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