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。
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.
出处
《贵州地质》
2008年第4期247-250,共4页
Guizhou Geology
关键词
梅树村期
黑色岩系
多金属矿
沉积地质特征
Meishucun period
black rock series
polymetal ore
sedimentary geologic character
