| 云南景东文玉火山热液型铜矿 |
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| 引用本文： | 王应宝,杨志东,李云留.云南景东文玉火山热液型铜矿[J].云南地质,2009,28(1):56-59. |
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| 作者姓名： | 王应宝 杨志东 李云留 |
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| 作者单位： | 云南地矿建设工程总公司普洱分公司,云南普洱,665000 |
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| 摘 要： | 铜矿赋存在三叠系上统小定西组火山岩系中，岩浆期后热液对矿质的运移、改造、叠加起重要作用。矿床具中低温火山热液蚀变特征。
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| 关 键 词： | 火山热液 中低温蚀变 叠加改造 云南景东文玉铜矿 |
THE WENYU VOLCANIC HYDROTHERMAL CU DEPOSIT IN JINGDONG, YUNNAN |
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| WANG Ying-bao,YANG Zhi-dong,LI Yun-liu.THE WENYU VOLCANIC HYDROTHERMAL CU DEPOSIT IN JINGDONG, YUNNAN[J].Yunnan Geology,2009,28(1):56-59. |
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| Authors: | WANG Ying-bao YANG Zhi-dong LI Yun-liu |
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| Institution: | ( Puer Branch, Yunnan Company of Construction Engineering of Geology ＆ Mineral Resources, Puer 665000 ) |
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| Abstract: | The Cu deposit exists in the Upper Triassic Xiaodingxi Formation volcanic rock seties. The postmagmatic thermal fluid plays an important part in transportation, reformation and superimposition of ore elements. The ore deposit has the characteristics of middle - low T volcanic hydrothermal alteration. |
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| Keywords: | Volcanic Thermal Fluid Middle -Low T alteration Superimposition -Reformation Wenyu Cu Deposit Jingdong Yunnan |
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