| 云南沧源羊缅金矿成因 |
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| 引用本文： | 高李阳,王爱萍.云南沧源羊缅金矿成因[J].云南地质,2011,30(3):273-274. |
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| 作者姓名： | 高李阳 王爱萍 |
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| 作者单位： | 云南黄金矿业集团股份有限公司,昆明,650224 |
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| 摘 要： | 羊缅金矿位于昌宁-孟连有色金属贵金属成矿带，金矿受压扭性断裂控制，分布于变余辉长辉绿岩中，典型的低温热液蚀变型金矿床。
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| 关 键 词： | 热液蚀变金矿 构造破碎带 辉绿辉长岩中 云南沧源羊缅 |
THE GENESIS OF YANGMIAN AU DEPOSIT IN CANGYUAN, YUNNAN |
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| GAO Li-yang,WANG Ai-ping.THE GENESIS OF YANGMIAN AU DEPOSIT IN CANGYUAN, YUNNAN[J].Yunnan Geology,2011,30(3):273-274. |
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| Authors: | GAO Li-yang WANG Ai-ping |
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| Institution: | GAO Li-yang,WANG Ai-ping(Yunnan Au Mining Group,Kunming 650224) |
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| Abstract: | The Yangrnian Au deposit is in the Changning--Menglian nonferrous- precious metal metalloge- netie zone. The ore deposit is controlled by the pressure - twisting fault, in the blastogabbroic diabase, which be-longs to the typical low T hydrothermal alteration Au deposit. |
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| Keywords: | Hydrothermal Alteration Au Deposit Structural Fractured Zone Diabase - Gabbro Yangmi-an Cangyuan Yunnan |
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