| 云南金平银厂坡金矿成矿模式 |
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| 引用本文： | 蔡培全,何忠福,吴文辉.云南金平银厂坡金矿成矿模式[J].云南地质,2010,29(2):168-171. |
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| 作者姓名： | 蔡培全 何忠福 吴文辉 |
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| 作者单位： | 1. 云南黄金矿业集团股份有限公司,昆明,650224
2. 云南鹤庆北衙矿业有限公司,大理,北衙,671000 |
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| 摘 要： | 银厂坡金矿位于金平断凹西部哀牢山深大断裂南缘。控矿因素为地层、构造、岩浆岩。为岩浆期后热液通过富集作用形成的残坡积土型金矿。系统介绍银厂坡金矿地质特征和成矿规律,给出该区理想的成矿模式。
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| 关 键 词： | 残坡积型金矿 微粒自然金 控矿因素 金矿成矿模式 云南金平银厂坡 |
THE METALLOGENETIC MODEL OF YINCHANGPO AU DEPOSIT IN JINPING,YUNNAN |
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| CAI Pei-quan,HE Zhong-fu,WU Wen-hui.THE METALLOGENETIC MODEL OF YINCHANGPO AU DEPOSIT IN JINPING,YUNNAN[J].Yunnan Geology,2010,29(2):168-171. |
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| Authors: | CAI Pei-quan HE Zhong-fu WU Wen-hui |
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| Institution: | 1.Yunnan Au Mining Company(Group),Kunming 650224;2.Beiya Mining Company(Ltd) of Heqing,671000) |
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| Abstract: | The Yinchangpo Au deposit is located along the S margin of Ailaoshan megafault in the W part of Jinping fault sag.The ore control factor includes strata,structure and magmatic rock.It is the eluvial-slope wash Au deposit formed by the postmagmatic hydrothermal enrichment.In this paper,we introduce systematically the geological characteristics,metallogenetic rule of Yinchangpo Au deposit and the ideal metallogenetic model of this orefield. |
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| Keywords: | Eluvial-Slope Wash Au Deposit Micrograined Natural Au Ore Control Factor Metallogenetic Model of Au Deposit Yinchangpo Jinping Yunnan |
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