Geological features and ore-controlling conditions of sand stone (conglomerate)copper deposit in Kumukuli basin, Xinjiang

The Kumukuli sandst one (conglomerate) copper deposit is located in western segment of East Kunlun orogenic belt,Xinjiang.The strata of ore-bearing are composed of Oligocene Shimagou Formation,Miocene Shibiliang Formation and Pliocene Hong shiliang Formation.The orebelt is 170 km in length of EW and 10-60 km in width of SN.The mineralization was controlled by structures,lithology,lithofacies and paleog eography and paleoclimate.The mineralization type is continental sandstone (conglomerate) copper deposit.