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| 贵州梅树村期多金属矿沉积地质特征 | |
| 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) |
| 作者姓名： | 谢海 王天华 曾湘贵 |
| 作者单位： | 贵州黔源地矿工程技术咨询有限公司,贵州,贵阳,550000;贵州省地矿局区域地质调查研究院,贵州,贵阳,550005 |
| 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。 |
| 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) | |
| Authors: | XIE Hai WANG Tian-hua CAO Xiang-gui |
| 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. |
| Keywords: | Meishucun period black rock series polymetal ore sedimentary geologic character |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ | |