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内蒙古翁牛特旗南湾子大地构造位置处于华北板块内蒙古中部地槽褶皱系温都尔庙~翁牛特旗加里东地槽褶皱带。该区地质构造复杂,内生金属矿产丰富。金、银矿产于石英脉体内或构造破碎带中,受构造控制。矿区附近铅锌矿较多,多集中在少郎河南岸,主要矿产为铅锌矿。通过对该区的区域地质特征和矿区地质特征分析,确定本区内银金多金属矿产资源潜力。
Inner Mongolia Wengniute Banner Nanwanzi tectonic location in the North China plate in Inner Mongolia geosynclinal fold Wengduerdal ~ Wengniute Banner Galliferong Trough fold belt. The geological structure of the complex, rich in endogenous metal minerals. Gold, silver minerals in the quartz vein body or the structure of the broken zone, controlled by the structure. There are many lead-zinc mines near the mining area, mostly concentrated in the southern bank of Shaolin River. The main mineral is lead-zinc mine. Through the analysis of the regional geological characteristics and geological characteristics of the area, the potential of silver, gold and polymetallic mineral resources in this area can be determined.