| 云南保山黄家地石英脉型金矿床成因 |
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| 引用本文： | 赵成峰,胡光道.云南保山黄家地石英脉型金矿床成因[J].云南地质,2008,27(4):442-447. |
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| 作者姓名： | 赵成峰 胡光道 |
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| 作者单位： | 1. 中国地质大学(武汉)资源学院,湖北,武汉,430074;云南地矿资源股份有限公司,云南,昆明,650215
2. 中国地质大学(武汉)资源学院,湖北,武汉,430074 |
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| 摘 要： | 金矿体明显受断裂构造及石英脉体的双重控制。根据矿床地质特征分析，认为该矿床成因为沿构造劈理充填、改造的中低温低硫热液石英含金硫化物复合脉型矿床，具中一大型远景规模。
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| 关 键 词： | 石英脉型 金矿床 多期次多来源 构造破碎带 保山地块 云南 |
THE GENESIS OF HUANGJIADI AU DEPOSIT OF QUARTZ VEIN TYPE IN BAOSHAN, YUNNAN |
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| ZHAO Cheng-feng,HU Guang-dao.THE GENESIS OF HUANGJIADI AU DEPOSIT OF QUARTZ VEIN TYPE IN BAOSHAN, YUNNAN[J].Yunnan Geology,2008,27(4):442-447. |
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| Authors: | ZHAO Cheng-feng HU Guang-dao |
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| Institution: | ZHAO Cheng-feng HU Guang-dao ( 1. Resource College, China University of Geosciences, Wuhan 430074 2. Yunnan Company of Geology and Mineral Resources, Kunming 650215 ) |
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| Abstract: | The Au orebody is evidently controlled by both fault and quartz vein.According to the analysis of geological characteristics,we believe that this ore deposit belongs to the reformed middle-low T hydrothermal deposit of quartz and Au-bearing sulfid composite vein(filling along structural cleavage) type,with a large potential scale. |
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| Keywords: | Au Deposit of Quartz Vein Type Multiphase and Polygene Structural Fracture Zone Baoshan Massif West Yunnan |
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