The Changren copper-nickel deposit hosts in ∑11 rock body and the rock occurrences in Changren-Qinglong fracture NNE compresso-shear tectonic belt. The surrounding rock is the lower strata of Qinglongchun Group of Ordovician. The rock body shows stock lens-shaped. The contact plane of rock bodies and surrounding rocks show leisure shape ore bodies occur in ∑11 ultra-thin pyroxene olive rock-olive rock bearing pyroxene olives, showing lay-like, lenticular structure. It is preliminary considered that deposit belongs to late magmatic melt-penetration one in genesis.