Abstract:Based on data of Saishitang copper mining area, it proved that there have orebearing porphyries and peripheral dike swarm. The orebearing porphyries are Calcalkaline-highK Calcalkaline-Shoshonitie, coexistence with adakitelike rocks, the ISr (0.7060~0.7086) is similar to the basic rocks and enclaves of later Ttriassic in east Kunlun area, 143Nd/144Nd(0.512226~0.512350) is closed to the adakitelike rocks which formed by basaltic lower crustal melting. The porphyries have a relative with the mantlederived magma from the enrichment mantle II,and the metallogenic background is related to the magmatic underplating at later Triassic in east Kunlun area. The shallowseated phase of orebearing intermediateacid stock are living high level with the dike swarm and subvolcanic rock. There have classical porphyritic mineralized alteration with centered orebearing porphyries. The mineralization has several stages and orebearing mainly of porphyries, meanwhile including of skarns, vein rocks, apophysis and breccia. Although we have found few porphyries currently, and can not completely know their characteristics, yet the thick and big porphyry is an important characteristics which can not be ignored. Porphyrytype is symbiosis with skarntype and hydrothermaltype, which have the characteristics of porphyry metallogenic series. Compared with the porphyry copper ore deposit in the world, it believed that the gensis of Saishitang copper deposit is a porphyry superposition compound ore deposit.