| 翁嘎科金矿矿床成因及找矿标志 |
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| 引用本文： | 金荣明. 翁嘎科金矿矿床成因及找矿标志[J]. 云南地质, 2008, 27(4): 437-441 |
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| 作者姓名： | 金荣明 |
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| 作者单位： | 云南地勘局物化探队,昆明,宜良,652100 |
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| 摘 要： | 金矿赋存在西盟群王雅组第四段第一、二亚段地层和次级断裂裂隙中。从地质特征、矿体赋存状态、矿石特征等判断，矿床成因类型为热液充填交代型。而北东向区域断裂中，可能找到新的矿体。
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| 关 键 词： | 含金石英脉 构造破碎带 王雅组第四段 小而富金矿 西盟翁嘎科云南 |
THE GENESIS AND PROSPECTING OF WENGGAKE AU DEPOSIT |
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| JIN Rong-ming. THE GENESIS AND PROSPECTING OF WENGGAKE AU DEPOSIT[J]. Yunnan Geology, 2008, 27(4): 437-441 |
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| Authors: | JIN Rong-ming |
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| Affiliation: | JIN Rong-ming (Geophysical ＆ Geochemical Exploration Team, Yunnan Bureau of Geology ＆ Mineral Resources, Yiliang 652100) |
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| Abstract: | The Au deposit is situated in the Member 4 of Wangya Formation and the secondary fault fissure.According to the analysis of geological characteristics,occurrence of ore body and ore characteristics,etc,it belongs to the ore deposit of hydrothermal filling-metasomatic type.The new ore body can be found out in the NE regional fault. |
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| Keywords: | Au-Bearing Quartz Vein Structural Fracture Zone Member 4 of Wangya Formation Small-Rich Au Deposit Wenggake Ximeng Yunnan |
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