ObjectivernThe Zhongdian area, Yunnan Province, is located in the southern of the Yidun Island arc belt in the Tethys-Himalayan metallogenic area, and is one of the important copper polymetallic mineral resource bases in China.Based on the previous studies (Liu et al., 2014), this paper discusses the Late Cretaceous tectono-thermal events in Zhongdian, to reconstruct the framework of their evolution and to restore the uplift history of representative oreforming porphyries.