| 四川康定县贵台子金矿地质特征及成因模式 |
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| 引用本文： | 和玉红.四川康定县贵台子金矿地质特征及成因模式[J].云南地质,2014(4):583-587. |
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| 作者姓名： | 和玉红 |
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| 作者单位： | 云南南方地勘工程总公司,云南大理671000 |
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| 摘 要： | 康定贵台子金矿位于大渡河金多金属成矿远景区中段,矿体主要受构造及岩浆岩控制,成矿流体来自深部,矿床类型属石英脉型金矿.在康定杂岩高含金性的基础上,通过中—新生代以来的构造—热事件作用,金元素再次活化富集和迁移.在有利部位重新就位形成工业矿体.
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| 关 键 词： | 石英脉型金矿 控矿构造 四川康定贵台子 |
THE GEOLOGICAL FEATURE AND GENESIS MODEL OF GUITAIZI AU DEPOSIT IN KANGDING,SICHUAN |
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| HE Yu-hong.THE GEOLOGICAL FEATURE AND GENESIS MODEL OF GUITAIZI AU DEPOSIT IN KANGDING,SICHUAN[J].Yunnan Geology,2014(4):583-587. |
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| Authors: | HE Yu-hong |
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| Institution: | HE Yu-hong ( Yunnan South Geoexploration Company General, Dali 671000) |
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| Abstract: | Guitaizi Au deposit, Kangding is in the middle section of Daduhe Au mulhmetalhc metatlogenesis perspective region. The orebody is controlled mainly by the structure and magrnatic rock. The metallogenetic fluid is derived from the deep. It belongs to the Au deposit of quartz vein type. Based upon the Au high Kangding com- plex, owing to Mesozoic-Cenozoic structure-heat event, Au activation, concentration and and migration again, emplacement in advantageous site and forming the commercial orebody. |
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| Keywords: | Au Deposit of Quartz Vein Type Ore Control Structure Guitaizi Kangding Sichuan |
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