| 新疆铜沟矿区矿床地质特征及成矿机制 |
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| 引用本文： | 张锐.新疆铜沟矿区矿床地质特征及成矿机制[J].岩土工程界,1997(6). |
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| 作者姓名： | 张锐 |
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| 作者单位： | 有色总公司新疆地勘局物探大队 |
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| 摘 要： | 简述了柴窝堡铜矿带西段铜沟矿区的地质特征。矿区受地层层位控制的似层状矿体和受断裂控制的矿体分别属海底喷流沉积成矿和岩浆期后成矿热液充填断裂成矿，为不同成矿期、不同成矿方式、有一定成因联系的多因复成矿床。
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| 关 键 词： | 铜矿 成矿机制 新疆 |
GEOLOGY AND METALLOGENIC MECHANISM OF THE TONGGOU DEPOSIT, XINJIANG |
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| Zhang Rui.GEOLOGY AND METALLOGENIC MECHANISM OF THE TONGGOU DEPOSIT, XINJIANG[J].Geotechnical Engineering World,1997(6). |
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| Authors: | Zhang Rui |
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| Abstract: | The study of geology of the Chaiwopu copper belt shows that the quasi strata form ore bodies controlled by strata and ore bodies controlled by faults were formed by fluid exhalation on sea bed and hydrothermal fiuid filling of post magmatic actives. It is considered to be a complex deposit formed in different periods and in different metallogenic style. |
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| Keywords: | Cu ore deposit metallogenic mechanism Xinjiang |
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