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一、矿区地质概况铜花山钴—多金属矿区位于托克逊县库米什东南23公里处。构造上属天山地槽南天山地向斜褶皱带。区内构造复杂,断裂发育,以北西西向压扭性断裂为主,次有北北东或北东东向断裂。矿区出露地层为中泥盆统阿拉塔格组的浅海相碎屑岩。因变质作用的影响,碎屑岩变为千枚岩、绢云母石英片岩和绢云母绿泥石片岩;灰岩变为大理岩成钙质片岩。铜花山超
First, the geological overview of mining area Tonghuashan cobalt - polymetallic mining area is located 23 km southeast of Qushishushun County. Structure on the Tianshan Trough southern Tianshan mountain syncline fold belt. The structure is complex in the area with the development of faults, mainly in the northwesterly and west-direction compressive-shear faults, and the sub-faults are north-north east or northeast-east. The exposed area of the mine area is a shallow marine clastic rock of the Middle Devonian Araratage. Due to metamorphism, clastic rocks into phyllite, sericite quartz schist and sericite chlorite schist, and limestone into marble into calcareous schist. Copper flowers super