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    刘国范, 朱广彬, 陈金铎, 杨振军, 秦爽. 新疆阿尔金南缘断裂带铜金铂钯贵金属矿床特征及成因[J]. 地质与资源, 2005, 14(1): 28-32. DOI: 10.13686/j.cnki.dzyzy.2005.01.007
    引用本文: 刘国范, 朱广彬, 陈金铎, 杨振军, 秦爽. 新疆阿尔金南缘断裂带铜金铂钯贵金属矿床特征及成因[J]. 地质与资源, 2005, 14(1): 28-32. DOI: 10.13686/j.cnki.dzyzy.2005.01.007
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    LIU Guo-fan, ZHU Guang-bin, CHEN Jin-duo, YANG Zhen-jun, QIN Shuang. GEOLOGY AND METALLOGENESIS OF THE PRECIOUS METAL DEPOSITS IN THE SOUTH MARGIN FAULT ZONE OF ALTUN MOUNTAIN, XINJIANG[J]. Geology and Resources, 2005, 14(1): 28-32. DOI: 10.13686/j.cnki.dzyzy.2005.01.007
    Citation: LIU Guo-fan, ZHU Guang-bin, CHEN Jin-duo, YANG Zhen-jun, QIN Shuang. GEOLOGY AND METALLOGENESIS OF THE PRECIOUS METAL DEPOSITS IN THE SOUTH MARGIN FAULT ZONE OF ALTUN MOUNTAIN, XINJIANG[J]. Geology and Resources, 2005, 14(1): 28-32. DOI: 10.13686/j.cnki.dzyzy.2005.01.007
    shu

    新疆阿尔金南缘断裂带铜金铂钯贵金属矿床特征及成因

    GEOLOGY AND METALLOGENESIS OF THE PRECIOUS METAL DEPOSITS IN THE SOUTH MARGIN FAULT ZONE OF ALTUN MOUNTAIN, XINJIANG

      摘要
    • 摘要: 阿尔金南缘断裂是一条深达上地幔的区域性大断裂,沿断裂分布着众多的基性-超基性杂岩体.岩浆结晶分异晚期,铜、金、铂、钯元素富集,在后期构造热液作用下,形成了清水泉等处的铜、金、铂、钯工业矿床.阿尔金一带找矿前景极大.

       

      Abstract: The south margin faulted zone of Altun Mountain in Xinjiang is a regional upper mantle deep structure,along which numerous basic-ultrabasic complex bodies are distributed.The elements of Cu,Au,Pt and Pd are concentrated in the late stage of magmatic crystallization and differentiation.With later tectonic hydrothermal process,commercial copper-gold-platinum-palladium deposits are formed in Qingshuiquan and other places.There is a great potential for the exploration in Altun area.

       

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