Geological Characteristics and Prospecting Indicators of Senji Molybdenum Ore Body in Urad Houqi, Inner Mongolia Based on geological mapping, soil geochemical survey, surface trough exploration and deep drilling verif...Geological Characteristics and Prospecting Indicators of Senji Molybdenum Ore Body in Urad Houqi, Inner Mongolia Based on geological mapping, soil geochemical survey, surface trough exploration and deep drilling verification and control, the Senji Molybdenum deposit was discovered. Geological characteristics of the molybdenum ore body are described. The host lithology of molyb</span><span style="font-family:Verdana;">denum ore body is mainly in the cataclastic carbonated black plagioclase </span><span style="font-family:Verdana;">gneiss of the second rock member of the Paleoproterozoic Baoyintu Group, followed by Early Carboniferous monzogranite. The genetic type of the </span><span style="font-family:Verdana;">deposit is preliminarily deduced to be a hydrothermal filling vein-type</span><span style="font-family:Verdana;"> molybdenum </span><span style="font-family:Verdana;">deposit. The significance of this paper is to summarize the prospecting</span><span style="font-family:Verdana;"> marks of the molybdenum ore body in this area, so as to further guide the exploration work in this area, and at the same time provide a useful reference for the exploration work of similar deposits in other areas.展开更多
文摘Geological Characteristics and Prospecting Indicators of Senji Molybdenum Ore Body in Urad Houqi, Inner Mongolia Based on geological mapping, soil geochemical survey, surface trough exploration and deep drilling verification and control, the Senji Molybdenum deposit was discovered. Geological characteristics of the molybdenum ore body are described. The host lithology of molyb</span><span style="font-family:Verdana;">denum ore body is mainly in the cataclastic carbonated black plagioclase </span><span style="font-family:Verdana;">gneiss of the second rock member of the Paleoproterozoic Baoyintu Group, followed by Early Carboniferous monzogranite. The genetic type of the </span><span style="font-family:Verdana;">deposit is preliminarily deduced to be a hydrothermal filling vein-type</span><span style="font-family:Verdana;"> molybdenum </span><span style="font-family:Verdana;">deposit. The significance of this paper is to summarize the prospecting</span><span style="font-family:Verdana;"> marks of the molybdenum ore body in this area, so as to further guide the exploration work in this area, and at the same time provide a useful reference for the exploration work of similar deposits in other areas.
