| 黄山铜镍硫化物矿床10号矿体形成机理及远景评价 |
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| 引用本文： | 阳正熙,唐菊兴.黄山铜镍硫化物矿床10号矿体形成机理及远景评价[J].矿物岩石,1996,16(1):44-50. |
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| 作者姓名： | 阳正熙 唐菊兴 |
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| 作者单位： | 成都理工学院矿床地质研究所 |
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| 摘 要： | 黄山铜镍矿床１０号矿体是赋存在镁铁－－超镁铁杂岩体内辉长苏长岩相中的浅富铜镍矿体，它是由含有高温气态的硫化物熔浆贯入－－硫化作用成矿。矿体形成后受到成矿后断层的破坏。
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| 关 键 词： | 铜矿床 镍矿床 矿体形成机理 |
METALLOGENIC MECHANISM AND PROSPECTIVE VALUE FOR NO. 10 OREBODYIN HUANGSHAN Cu-Ni SULFIDE DEPOSIT |
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| Yang Zhengxi,Tang Juxing, Mou Jilu, Li Chengde.METALLOGENIC MECHANISM AND PROSPECTIVE VALUE FOR NO. 10 OREBODYIN HUANGSHAN Cu-Ni SULFIDE DEPOSIT[J].Journal of Mineralogy and Petrology,1996,16(1):44-50. |
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| Authors: | Yang Zhengxi Tang Juxing Mou Jilu Li Chengde |
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| Abstract: | NO. 10 orebody in Huangshan Cu-Ni sulfide deposit, Xinjiang,is an enriched and outcropped one located in the gabbonorite of Huangshan mafic-ultramafic complex. The orebody was formed by the injection and sulfidization of the remnant sulfide melt with high-temperature gaseous sulfur,and was faulted afterwards. |
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| Keywords: | Huangshan Cu-Ni metallogenic belt gabbonorite face |
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