| 西昆仑中间隆起带花岗岩及与铜金矿化关系 |
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| 引用本文： | 王书来,汪东波,祝新友.西昆仑中间隆起带花岗岩及与铜金矿化关系[J].矿产与地质,2000,14(1):5-10. |
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| 作者姓名： | 王书来 汪东波 祝新友 |
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| 作者单位： | 中国有色金属工业总公司北京矿产地质研究所,北京,100012 |
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| 基金项目： | 有色金属工业地质科研项目!96－ D－ 1 |
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| 摘 要： | 西昆仑中间隆真情喧是自震旦纪以来从塔里木板块裂解开来的古地体，花岗岩类稀土酚模式，微量元素特征表明形成于岛弧及挤压碰拦期和期后环境，金铜矿化与华力西期后花岗岩类关系较紧密。该区金铜找矿类型重点为斑岩铜金矿、矽卡岩型铜金矿、韧性剪切带型金矿及与斑岩脉有关的构造热液金矿。
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| 关 键 词： | 花岗岩 铜矿 金矿 矿化 西昆仑 隆起带 |
RELATIONSHIP BETWEEN GRANITES OF UPLIFT IN CENTRE-WESTERN KUNLUN MOUNTAIN AND Cu-Au MINERALZATION |
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| Wang Shulai,Wang Dongbo,Zhu Xinyou.RELATIONSHIP BETWEEN GRANITES OF UPLIFT IN CENTRE-WESTERN KUNLUN MOUNTAIN AND Cu-Au MINERALZATION[J].Mineral Resources and Geology,2000,14(1):5-10. |
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| Authors: | Wang Shulai Wang Dongbo Zhu Xinyou |
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| Abstract: | The uplift belt of center western kunlun mountain is an ancient plate derived from Talimu plate since sinian period. Distribution pattern of rare earth elements and characteristics of microelements reflect that Cu Au mineralization has a close relationship with granites of late variscon movement. The main kinds of Cu Au orebodies in this region are those of porphyry, skarn, tenacity shear belt and hydrothemal related with porphyry veins. |
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| Keywords: | Granite Cu Au orebody west kunlun mountain Xinjiang |
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