| 云南维西格坡洛斑岩型锑矿矿床成因 |
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| 引用本文： | 蒋志荣,罗显辉.云南维西格坡洛斑岩型锑矿矿床成因[J].云南地质,2009,28(3):259-262. |
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| 作者姓名： | 蒋志荣 罗显辉 |
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| 作者单位： | 云南省有色地质楚雄勘查院,云南,楚雄,675000 |
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| 摘 要： | 锑矿化集中于喜马拉雅期石英斑岩内接触带，存在矿源层形成、充分分异及近地表成矿三个阶段。可作为滇西碱性岩锡矿床典型。
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| 关 键 词： | 脉状锑矿化 热液裂隙充填 碱性石英斑岩 两类容矿空间 云南维西格 |
ON THE GENESIS OF GEPOLUO PORPHYRY SB DEPOSIT IN WEIXI, YUNNAN |
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| JIANG Zhi-rong,LUO Xian-hui.ON THE GENESIS OF GEPOLUO PORPHYRY SB DEPOSIT IN WEIXI, YUNNAN[J].Yunnan Geology,2009,28(3):259-262. |
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| Authors: | JIANG Zhi-rong LUO Xian-hui |
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| Institution: | ( Chuxiong Exploration Institute of Nonferrous Geology of Yunnan, Chuxiong 675000) |
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| Abstract: | The Sb metallogenesis is concentrated in the inner contact zone of Himalayan quartz porphyry. The formation process can be divided into the following 3 stages, ie 1. the formation of ore source bed; 2. the full differentiation; 3. the epigenetic metallogenesis. It can be regarded as the typical Sb deposit related to the alkaline rock in West Yunnan. |
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| Keywords: | Vein Sb Metallogenesis Hydrothermal Fissure Filling Alkaline Quartz Porphyry Ore - Bearing Space of 2 Types Gepoluo of Weixi Yunnan |
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