Information based on extensive investigation of mineral resources in recent years, the Tibet autonomous region and the Tibet autonomous regional mineral resources potential evaluation research on the system, detailed mineral resources information, writing discusses the Greatgandise northern Tibet, （including the Bangonhu-nujiang metallogenic belt, the North gandise metallogenic belt and Middle gandise metallogenic belt three metallogenic belts) of mineral geological characteristics and distribution regularity of mineralization and metallogenic series. The Bangonhu-nujiang metallogenic belt including the early yanshan (ocean basin forming period, such as DonqiaoCr deposit) and yanshan period (intracontinental subduction extrusion, such as WusolaAu deposit) magmatism related deposit metallogenic series and the Naqu-lolung basin related to the Himalayan period fluid effect, such as NaduolonPb deposit metallogenic series; Ore deposits are mainly distributed in the metallogenic belt of Shenza-Jiali line north (also known as the Gandise north ore belt), including the YugulaNi deposit (early yanshan, the magmatic rock type),the ShesuoCu deposit (yanshan period, mainly skarn type), Youcalarn-AngzhangPb deposit (mainly yanshan period, hydrothermal type), and ElongaAs deposit (early and late yanshanian and Himalayan fluid-type transformation mainly) four areas where different types of ore deposit metallogenic series; Middle gandise metallogenic belt in the near east-west two metallogenic belt, and the Geiji-xiongba-wenbu ore-forming subzone north's of yanshan period (such as GarqongCuAu ore deposit) Shiquanghe-shengza arc-basin evolution stage of magmatic hydrothermal mineralization metallogenic series of ore deposits, the south's Langjiu-tarochuo-namuchuo ore-forming subzone Himalayan period (such as JiagangWMoBi deposit) ore deposit metallogenic series of magmatic hydrothermal mineralization.