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马关县高井槽矿区位于杨子板块次级构造单元———屏边———西畴山弧区西南侧,南温河变质核杂岩构造西部,区内大范围出露酸性侵入岩南捞片麻岩。矿区出露的地层有:第四系与上元古界新寨组。断裂构造发育,剥离断层为主要容矿及控矿构造,矿化以白钨矿为主。沿剥离断层带是寻找钨多金属矿体的有利部位。
Gao Guanghuang Maguan Guanghuang area is located in the sub-unit Yangzi plate --- screen --- Xizhoushan arc area on the southwest side of the South Wenjiang metamorphic core complex structure of the western region exposed a wide range of acidic intrusive rocks Fishing gneiss. Stratum exposed areas are: the Quaternary and the Proterozoic Xinzhai group. Fracture structure development, stripping the fault as the main content of ore and ore control structure, mainly scheelite mineralization. Dislocation along the fault zone is looking for tungsten polymetallic ore favorable sites.