| 云南元阳大坪金矿矿床成因讨论 |
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| 引用本文： | 刘玉昆.云南元阳大坪金矿矿床成因讨论[J].云南地质,2013(4):386-388. |
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| 作者姓名： | 刘玉昆 |
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| 作者单位： | 云南环复地质有限公司,云南昆明650051 |
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| 摘 要： | 金矿位于哀牢山构造变质岩带、金（贵金属）成矿带南部西侧,含金石英脉分布于小新街断裂两侧的次级构造裂隙中,矿脉严格受次级压扭性断裂控制.
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| 关 键 词： | 石英脉型金矿 次级断裂控矿 成矿流体 深源矿质 云南元阳大坪 |
A DISCUSSION ABOUT THE GENESIS OF DAPING AU DEPOSIT IN YUANYANG,YUNNAN |
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| LIU Yu-kun.A DISCUSSION ABOUT THE GENESIS OF DAPING AU DEPOSIT IN YUANYANG,YUNNAN[J].Yunnan Geology,2013(4):386-388. |
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| Authors: | LIU Yu-kun |
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| Institution: | LIU Yu-kun ( Yunnan Huanfu Geological Company (Ltd) , Kunming 650051 ) |
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| Abstract: | The Au deposit is on the W side of S section of Ailaoshan tectonic metamorphic zone - - Au cious metal） metallogenetic zone. The Au - bearing quartz vein is in the secondary structural fissures of both of Xiaoxinjie fault, which is strictly controlled by secondary pressure - torsion fault. （ pre- sides |
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| Keywords: | Au Deposit of Quartz Vein Type Ore Control of Secondary Fault Metallogenetic Fluid DeepDerivation Ore Material Daping Yuanyang Yunnan |
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