| 云南双江大亮山金矿控矿因素及成因分析 |
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| 引用本文： | 花仁忠,王琨,龙洋,伏聪.云南双江大亮山金矿控矿因素及成因分析[J].云南地质,2013(4):379-381. |
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| 作者姓名： | 花仁忠 王琨 龙洋 伏聪 |
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| 作者单位： | [1]云南地矿总公司（集团）地质矿产勘查二院,云南昆明650051 [2]云南省地质矿产勘查开发局第一地质大队,云南曲靖655000 [3]云南宝泉矿业公司,云南昆明650051 |
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| 摘 要： | 矿体赋存于韧性剪切带,矿化带近南北向分布,为岩浆期后中—低温热液通过富集作用形成的微粒、浸染型金矿.
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| 关 键 词： | 中—低温热液型 脆—韧性剪切带 控矿因素 大亮山金矿 云南双江大亮山 |
AN ANALYSIS OF THE ORE CONTROL FACTOR AND THE GENESIS OF DALIANGSHAN AU DEPOSIT IN SHUANGJIANG,YUNNAN |
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| HUA Ren-zhong,WANG Kun,LONG Yang,FU Cong.AN ANALYSIS OF THE ORE CONTROL FACTOR AND THE GENESIS OF DALIANGSHAN AU DEPOSIT IN SHUANGJIANG,YUNNAN[J].Yunnan Geology,2013(4):379-381. |
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| Authors: | HUA Ren-zhong WANG Kun LONG Yang FU Cong |
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| Institution: | Exploration Institute 2 of Geology ＆ Mineral Resources, Yunnan Company (Group) of Geology ＆ Mineral Resources General, Kunming 650224) Yunnan Exploration ＆ Development Bureau of Geology ＆ Mineral Resources, Qujing 655000) (3. Yunnan Baoquan Mining Company, Kunming 650051 ) |
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| Abstract: | The ore body is in the ductile shear zone, and the metallogenesis zone is nearly NS - ward. It is a micro - grained disseminated Au deposit formed by the concentration of postmagmatic middle - low T thermal fluid. |
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| Keywords: | Middle -Low T Hydrothermal Type Brittle -Ductile Shear Zone Ore Control Factor Daliangshan Au Deposit Daliangshan Shuangjiang Yunnan |
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