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西昆仑中间隆起带是自震旦纪以来从塔里木板块裂解开来的古地体，花岗岩类稀土配分模式，微量元素特征表明形成于岛弧及挤压碰撞期和期后环境，金铜矿化与华力西期后花岗岩类关系较紧密。该区金铜找矿类型重点为斑岩铜金矿、矽卡岩型铜金矿、韧性剪切带型金矿及与斑岩脉有关的构造热液金矿。
The western Kunlun Mountains uplift belt is an ancient palaeosol cracked from the Tarim plate since the Sinian. The granite-like REE patterns and trace element characteristics indicate that the formation of the arcuate argillite during the island arc, It is closely related to the granite classes after the Variscan period. The gold-copper deposit types in this area are mainly porphyry copper-gold deposits, skarn copper-gold deposits, ductile-shear-type gold deposits and structural hydrothermal gold deposits related to porphyry veins.