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新疆萨热克大型砂砾岩型铜多金属矿床位于西南天山造山带,受萨热克巴依中生代陆内拉分盆地控制显著。该区出露中元古界阿克苏岩群、志留系、下侏罗统莎里塔什组和康苏组、中侏罗统杨叶组和塔尔尕组、上侏罗统库孜贡苏组和下白垩统克孜勒苏群,库孜贡苏组为赋矿层位(刘增仁等,2010)。萨热克裙边式复式向斜的北南两翼控制了北矿带和南矿带,北矿带控制长大于4000 m,平均宽5~80 m,铜矿(化)体产于库孜贡苏组上段(J3k2),呈NE-SW向延展,现已圈定了Ⅰ、Ⅱ-1、Ⅱ-2、Ⅱ-3等6个铜矿体。南矿
The Sagishike large conglomerate-type copper polymetallic deposit in Xinjiang is located in the southwestern Tianshan orogen and is under the control of the Saraikiba-Mesozoic Lunela sub-basin. In the area, the Aksu Group, the Silurian System, the Lower Jurassic Salitam Formation and the Kangsu Formation, the Middle Jurassic Yangye Formation and the Targa Formation, the Upper Jurassic Kuzigong Formation Su-group and Lower Cretaceous Kizilsu group and Ku-ki-gongsu formation are ore-bearing strata (Liu Zengren et al., 2010). The northern and southern oreblocks control the northern and southern oreblocks in the north-south wing of the Sagyg skirt-type double syncline. The control of the northern ore belt grows to more than 4,000 m with an average width of 5 to 80 m. The copper ore body is produced in the Kutigong The upper member of the Soviet Union (J3k2) extends in the NE-SW direction and has now delineated 6 copper ore bodies such as Ⅰ, Ⅱ-1, Ⅱ-2 and Ⅱ-3. South Mine