| 新疆阿尔金南缘断裂带铜金铂钯贵金属矿床特征及成因 |
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| 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. |
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| 作者姓名： | 刘国范 朱广彬 陈金铎 杨振军 秦爽 |
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| 作者单位： | 河南省地质调査院, 河南郑州 450007 |
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| 基金项目： | 中国地质调查局“新疆阿尔金南缘断裂带矿产资源调查评价”项目(编号20011020061)资助. |
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| 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.
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| 关 键 词： | 阿尔金南缘 铜、金、铂、钯矿床 基性-超基性杂岩 |
| 文章编号： | 1671-1947(2005)01-0028-05 |
| 收稿时间： | 2003-09-02 |
| 修稿时间： | 2003年9月2日 |
GEOLOGY AND METALLOGENESIS OF THE PRECIOUS METAL DEPOSITS IN THE SOUTH MARGIN FAULT ZONE OF ALTUN MOUNTAIN, XINJIANG |
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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. |
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| Authors: | LIU Guo-fan ZHU Guang-bin CHEN Jin-duo YANG Zhen-jun QIN Shuang |
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| Institution: | Henan Institute of Geological Survey, Zhengzhou 450007, China |
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| 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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| Keywords: | the south margin of Altun Mountain copper gold platinum palladium deposit basic ultrabasic complex |
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