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新疆阿尔金南缘断裂带铜金铂钯贵金属矿床特征及成因

Guo-fan LIU,Guang-bin ZHU, Jin-duo CHEN,Zhen-jun YANG,Shuang QIN

wf（2005）

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Abstract
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 .
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