摘要
文章通过对贵州清河黑色岩系中钼镍钒矿床地质特征、矿体及矿化特征、成矿地质条件进行分析认为,清河矿床具有典型沉积矿床的特征,矿体呈层状、似层状赋存于寒武系下统牛蹄塘底部炭质泥岩地层中。文章认为清河矿床受地层岩性、古构造和古地理条件、生物地球化学作用的控制。
Based on the analysis of the geological characteristics,ore bodies and mineralization characteristics of molybdenum-nickel-vanadium deposit in Qinghe black rock series,Guizhou Province,the authors believed that the Qinghe deposit has the characteristics of typical sedimentary deposits,and the ore bodies are layered.The layer-like occurs in the carbonaceous mudstone strata at the bottom of the Lower Cambrian Niujiutang.In this paper,it was considered that Qinghe deposit is controlled by stratigraphy,paleostructure,paleogeography and biogeochemistry.
作者
王承波
WANG Cheng-bo(Guizhou Geological Exploration Institute,China Chemical Geology and Mine Bureau,Guiyang,Guizhou 550000,China)
出处
《企业技术开发》
2019年第5期94-95,106,共3页
Technological Development of Enterprise
关键词
成矿地质条件
黑色页岩
钼镍钒
清河
贵州
Metallogenic geological conditions
Black shale
Mo,Ni,V
Qinghe
Guizhou