Abstract:Tianshuihai area in western Kunlun in Xinjiang Uygur Autonomous Region is located in QiaoertianshanChalukou fault zone. It is an important enrichment area of leadzinc deposits. The metallogenic geological conditions are superior, and more than ten deposits have been discovered. Through analyzing regional geological characteristics, geochemical characteristics and remote sensing anomaly characteristics of Tianshuihai area, two leadzinc minerogenic prospect are delineated. The rich ore location is mainly altered rock strata on the fault zone, and the deposit type focuses on the stratificationcontrolled leadzinc depsit. The prospecting signs are mainly Cretaceous or Jurassic strata around the structural fracture zone and Pb and Zn chemical element abnormal areas.