In this paper, geological and mineralization characteristics and metallogenetic model of Jinchuan Cu-Ni(PGE) magmatic sulfide deposit are systematically analysed and compared with Voisey’s Bay Cu-Ni(PGE) deposit(Canada), and the results show that the two world-class Cu-Ni(PGE) deposits have some common geological characteristics, and so, there are similarity and comparability on ore-forming and evaluation of the deposit. It is clarified that ore-bearing magma pulsating invasion and subsequent magma re-supply are very important ore-forming mechanism through which sulfide-bearing mafic-ultramafic magma assembles along the magma flowing conduit at depth to form super-larger Cu-Ni(PGE) magmatic sulfide deposits during the process of magmatic Ni-Cu sulfide deposits forming by “injecting of sulfide-bearing magma segregated at depth”. oft-com:office:office" />