| 贵州古风化壳沉积型铝土矿的沉积方式和成矿作用 |
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| 引用本文： | 盛章琪,廖莉萍.贵州古风化壳沉积型铝土矿的沉积方式和成矿作用[J].贵州地质,2010,27(4):255-258. |
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| 作者姓名： | 盛章琪 廖莉萍 |
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| 作者单位： | [1]贵州省地矿局地质科学研究所,贵州贵阳550004 [2]贵州省地质调查院,贵州贵阳550004 |
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| 摘 要： | 铝土矿沉积方式为胶体沉积及碎屑沉积,古红土化及沼泽化是形成铝土矿的主要成矿作用,地下潜水面以下200 m不是铝土矿深部找矿的红线。
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| 关 键 词： | 贵州 铝土矿 沉积 成矿作用 |
Sedimentary Mode and Mineralization of Sedimentary Bauxite Deposit of Fossil Weathering Crust in Guizhou |
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| SHENG Zhang-qi,LIAO Li-ping.Sedimentary Mode and Mineralization of Sedimentary Bauxite Deposit of Fossil Weathering Crust in Guizhou[J].Guizhou Geology,2010,27(4):255-258. |
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| Authors: | SHENG Zhang-qi LIAO Li-ping |
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| Institution: | 1.Institute of Geosciences,Guizhou Bureau of Geology and Mineral Exploration ＆ Development,Guiyang 550018,Guizhou,China;2.Guizhou Academy of Geologic Survey,Guiyang 550005,Guizhou,China) |
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| Abstract: | The sedimentary modes of bauxite deposit are colloid sediment and clastic sediment,fossil latefization and paludification are the main mineralization of the formation of bauxite deposit,200m under the water table is not the redline of deep exploitation. |
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| Keywords: | Guizhou bauxite deposit sediment mineralization |
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