| 新疆阿舍勒铜矿地质地球化学特征及构造控矿模拟实验 |
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| 引用本文： | 吴学益,李金铭.新疆阿舍勒铜矿地质地球化学特征及构造控矿模拟实验[J].矿物学报,1995,15(2):199-204,T001. |
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| 作者姓名： | 吴学益 李金铭 |
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| 作者单位： | 中国科学院地球化学研究所!贵阳，550002(吴学益，杨元根，王子江)，地质矿产部西安地质矿产研究所!西安，710054(李金铭，王长生) |
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| 摘 要： | 新疆阿舍勒铜矿是一个海底火山喷气－沉积的黄铁矿型铜矿床。地质地球化学特征研究表明，该矿床后期受褶皱、断裂构造影响，使铜矿在向斜倒转翼和向斜轴部增厚、加富，形成多次叠加的多因复成矿床。构造控矿模拟实验为阿舍勒铜矿的形成机理，提供了实验依据。
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| 关 键 词： | 铜矿床 模拟实验 控矿构造 地球化学 地质学 |
GEOLOGICAL AND GEOCHEMICAL CHARACTERISTICS OF THE ASHELE COPPER DEPOSIT,XINJIANG |
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| Wu Xueyi, Yang Yuangen, Wang Zijiang.GEOLOGICAL AND GEOCHEMICAL CHARACTERISTICS OF THE ASHELE COPPER DEPOSIT,XINJIANG[J].Acta Mineralogica Sinica,1995,15(2):199-204,T001. |
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| Authors: | Wu Xueyi Yang Yuangen Wang Zijiang |
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| Abstract: | The Ashele copper deposit in Xinjiang is a pyrite-type copper deposit of submarine volcano-ex-halative-sedimentary origin. Its geological and geochemical characteristics show that thle deposit has been thickened, enriched and repeatedly superimposed in the axial part of the syncline as a re-sult of the influence of folding and faulting at later stages. Simulating experiments on the struc-tural control over ore deposition provide the experimental grounds for the mechanism of formation of the Ashele copper deposit. |
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| Keywords: | Ashele characteristics of the copper deposit simulating experiment |
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