【摘要】 研究区位于东昆仑山中段,大地构造单元属东昆仑南坡俯冲增生杂岩带,是一个北西西向延伸的复合型俯冲碰撞杂岩带。区内断裂构造发育,F1是研究区内发育规模最大的一条断裂构造,控制着化探异常、矿化,金矿成因类型应为构造蚀变岩型金矿。化探、断裂构造、岩性、硅化脉等找矿标志明显,研究结果对以后的地质找矿工作具有很重要的指导意义。更多还原

【Abstract】 Located in the middle of the east kunlun mountains,the geotectonic unit belongs to the subduction and proliferation complex belt on the south slope of the east kunlun mountains. It is a complex subduction and collision complex belt extending from the north to the west. F1 is the largest fault structure developed in the study area,which controls geochemical anomaly and mineralization. The genesis type of gold deposit should be tectonic altered rock type gold deposit. Geochemical exploration,fault structure,lithology,silicate veins and other prospecting signs are obvious.更多还原