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内蒙狼山有色金属成矿带,面积约六千多平方公里.区内已探明的霍各乞、东升庙、炭窑口三大铜、铅、锌、硫多金属矿床,均属沉积变质矿床,受含矿层位严格控制.矿床具有沉积成矿和变质改造的特点. 区域地质特征狼山有色金属成矿带,处于蒙古地槽海西褶皱与中朝准地台交界带. 区域地层主要是上元古界狼山群浅变质岩系,局部有石炭系、二叠系、侏罗系、白垩系及第三系地层分布. 狼山群(Ptl)为本区含矿层,分为三个组(即
Inner Mongolia Langshan non-ferrous mineral metallogenic belt, an area of about more than 6000 square kilometers.Huobeiqi, Dongshengmiao, charcoal kiln mouth proven three copper, lead, zinc and sulfur polymetallic deposits, are sedimentary metamorphism The deposit is strictly controlled by the ore-bearing strata, and the deposit is characterized by sedimentary mineralization and metamorphism and alteration. The regional geological features include the Langshan non-ferrous metallogenic belt, which is located at the boundary between the Hercynian folds in Mongolia trench and the Sino-Korean quasi platform. Is the Proterozoic Langshan group of shallow metamorphic rocks, locally Carboniferous, Permian, Jurassic, Cretaceous and Tertiary stratigraphic distribution.Wolf Hill Group (Ptl) is the area containing the ore, divided into three Groups (ie