Large and super large ore deposits discovered to date in the plateau and its adjacent regions are spatially and temporally associated with the Himalayan collision orogenesis.

Mantle source characteristics of magmatic carbonatites from the Himalayan Collision Zone in western Sichuan,SW China:Evidence of Pb-Sr-Nd isotopes.;

Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry,exhumation history,and foreland sedimentation;

The uplift of the Himalayan orogen is an interesting geological problem.

The study area lying in the north slope of the middle part of Himalayan orogen involves abundant representative tectonic landforms.

The controls of the collisional orogenesis in the Qinling Mountains on the Carboniferous-Permian transgressional processes in North China;

The collisional orogenesis in the area occurred in the Carboniferous and Permian, and shows the character of the early compression and late extension.

The mineralizing time of skarn gold deposits is mainly of late Mesozoic (Yanshanian),contemporaneous with the collision orogenesis occurred in the mainland of China; the gold orebodies emplaced in the late stage of the collision orogenesis.