Based on the research of geochronology, the writer has determined the ages of Yeba volcanic rocks that in the Qulong—jiama ears, and Dirima intrusive rocks and Diuga granites, as well as the Ore bearing porphyry in Qulong and Xiangbeishan by Zircon U Pb LA ICP MS. And the results are 154.8±6.8Ma, 52.39±0.95Ma, 50.8±1.2Ma, 14.35±0.49Ma and 15.48±0.42Ma. Connecting the research of petrology and geochemistry, this paper studies the the space frame of tectonic—magmatic as well as the Mineralization of different stages in these areas. First of all, on the effect of Ocean—continent transition northward subduction of Neo Tethys Ocean, it has formed a broad region of the Yeba volcanic rocks. At this stage, the major subserieses include Cu—Au—Ag—Pb—Zn subeseries related to Early—Middle Jurassic arc type intermediate—felsic volcanic—supergene rock. Secondly, at ocean—continent collision conversion stage, it formed Linzizong Group volcanic and a lot of intrusive rocks. At this stage, it could help to create the Pb—Zn—Ag—Mo—W—Fe subseries related to Paleocene—Eocene intermediate—felsic volcanic rock and intermediate—supergene rock formation. Thirdly, in the post collisional period, at the mechanism of extension, a large number of ore bearing porphyry intrude upon the crust. At this stage, it could help to create the Cu—Mo—Pb—Zn—W—Au—Ag subseries related to Miocene intermediate—felsic supergene rock formation. They are the main mineralization types, and a large number of porphyry deposits were formed in Tibetan plateau as the result of collision between the India and the Lhasa plates.