| 云南绿春咪霞金矿成矿地质条件 |
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| 引用本文： | 普玉斌,杨玉华.云南绿春咪霞金矿成矿地质条件[J].云南地质,2008,27(3):325-330. |
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| 作者姓名： | 普玉斌 杨玉华 |
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| 作者单位： | 1. 云南省地质矿产勘查开发局滇南地质大队,云南,普洱,661600
2. 云南省有色地质院滇南院,云南,个旧,661000 |
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| 摘 要： | 咪霞金矿赋存在多元素高背景值下志留统薄层状蚀变板岩中，受北西向F6-1断裂及正长岩、煌斑岩控制，与多元素异常、黄铁矿化等多种围岩蚀变对应，具较好的成矿地质条件。
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| 关 键 词： | 层间破碎带 金异常 围岩蚀变 煌斑岩 咪霞绿春云南 |
THE METALLOGENETIC GEOLOGICAL CONDITIONS OF MIXIA AU DEPOSIT IN LUCHUN, YUNNAN |
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| PU Yu-bin,YANG Yu-hua.THE METALLOGENETIC GEOLOGICAL CONDITIONS OF MIXIA AU DEPOSIT IN LUCHUN, YUNNAN[J].Yunnan Geology,2008,27(3):325-330. |
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| Authors: | PU Yu-bin YANG Yu-hua |
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| Institution: | PU Yu-bin ,YANG Yu-hua (South Yunnan Geological Team, Yunnan Exploration and Development Bureau of Geology and Mineral Resources, Puer 661660) |
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| Abstract: | The Mixia Au deposit occurs in Lower Silurian thin bedded altered slate with high background value of multiple elements, which is controlled by NW fault F6 - 1 and syenite, lamprophyre. It is corresponding to anomaly of multiple elements and various wall rock alteration, such as pyritization, etc, which has good metallogenetic geological conditions. |
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| Keywords: | Bedding Fracture Zone Au Anomaly Wall Rock Alteration Lamprophyre Mixia Luchun Yunnan |
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