///Wangshe Cu-W deposit, located in Guangxi, is a porphyry type copper and molybdnium deposit, superimposed by quartz vein-type tungsten. Cu, Mo and W in the deposit are economic elements with an average Cu grade of more than 0.3%. It is preliminarily inferred that the geodynamic setting of late Yanshanian mineralization in this region is lower crustal delamination and lithospheric thinning.