| 一个大型红土型金矿的成矿地质条件及形成机理分析 |
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| 引用本文： | 虞人育.一个大型红土型金矿的成矿地质条件及形成机理分析[J].地质与勘探,1996,32(1):1-6,32. |
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| 作者姓名： | 虞人育 |
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| 作者单位： | 湖北省第四地质大队 |
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| 摘 要： | 蛇屋山金矿床是我国首先在湖北省发现并探明的大型红土型金矿床。矿床经渗流热卤水成矿作用，形成原生金矿化（体）；再经表生同化成矿作用形成风化型金矿床。矿床成因类型属渗流热卤水－表生成因的残积粘土型金矿床，工业类型为红土型金矿床。
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| 关 键 词： | 金矿床 红土型 成矿 地质条件 形成机理 |
Geological Conditions and Mechanism of Metallization of a Large-scal Laterite-type Gold Deposit |
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| Yu Renyu.Geological Conditions and Mechanism of Metallization of a Large-scal Laterite-type Gold Deposit[J].Geology and Prospecting,1996,32(1):1-6,32. |
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| Authors: | Yu Renyu |
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| Abstract: | Sheweishan gold deposit is a large-scale laterite-type deposit first found in Hubei Province of China.The deposit experienced vadose hot brine and formed original gold minerallization.And then through supergene weathering mineralllzation,weatheringtype gold deposit was formed.The deposit belongs to vadose hot brine-supergene genetic eluvial clay-type gold deposit and to laterite-type gold-deposit in terms of industry. |
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| Keywords: | vadose hot brine karst unconformity surface barrier structure weathering leaching uncombined gold lateritetype gold deposit |
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