| 贵州梅树村期多金属矿沉积地质特征 |
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| 引用本文： | 谢海,王天华,曾湘贵.贵州梅树村期多金属矿沉积地质特征[J].贵州地质,2008,25(4). |
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| 作者姓名： | 谢海 王天华 曾湘贵 |
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| 作者单位： | 1. 贵州黔源地矿工程技术咨询有限公司,贵州,贵阳,550000
2. 贵州省地矿局区域地质调查研究院,贵州,贵阳,550005 |
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| 摘 要： | 贵州早寒世武梅树村期黑色岩系黑色岩系中的Mo、Ni、V等多金属矿与沉积环境的关系密切,形成不同的多金属组合,可分为粘土岩型钼钒矿和黄铁矿型镍钼矿和粘土岩型钒矿三种组合,分布于不同的沉积相区,可能为深源物质封闭海域沉积作用的产物。
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| 关 键 词： | 梅树村期 黑色岩系 多金属矿 沉积地质特征 |
The Sedimentary Geologic Character of Polymetal Ore of Meishucun Period in Guizhou |
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| XIE Hai,WANG Tian-hua,CAO Xiang-gui.The Sedimentary Geologic Character of Polymetal Ore of Meishucun Period in Guizhou[J].Guizhou Geology,2008,25(4). |
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| Authors: | XIE Hai WANG Tian-hua CAO Xiang-gui |
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| Abstract: | Mo,Ni,V and other polymetals in black rock series in Meishucun period in early Cambrian in Guizhou close relationship with sedimentary environment,formed different polymetal associations: clayrock Mo,V ore,iron pyrites Ni,Mo ore and clayrock V ore.They distributed in sedimentary facies areas and may be the outcome of sedimentation of deep materials in close sea area. |
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| Keywords: | Meishucun period black rock series polymetal ore sedimentary geologic character |
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