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MINEROGENETIC MODEL OF THE JINCHUAN COPPER AND NICKEL SULFIDE DEPOSIT

Tang Zhongli (Geology and Mineral Rosources Bureau of Gansu Province)  
The Jinchuan deposit occurs in transitio regions. It is located in the Alashan uplift belt on the southwestern margin of the Sino-Korean landmass. The orebeari-ng rock bodies have been formed by intrusions and injections of magmas for many times. Its isotopic ages is 1508±31 Ma. The sulfur-rich ferruginous ultrabasic magma derived from the deep-seated mantle was intruded in the magma chamber of the deep levels of the crust along the ultracrustal fault. The magma underwent liquid unmixing and olivine crystalization in the magma chamber between the liquidus line temperature and the solidus line temperature. Due to gravity effect, the early-separated liquid(unmixed sulphideme-1t) was then localized in the Lower part, while the later-separated liquid(unmixed su-1fide melt)together with the crystallized olivine were localized in the upper part, forming the stratified sulfide ore magma, sulfide-rich magma, sulfide-bearing magma andesilica-temagma upward in the magma chamber. As the temperature fell down, in process of the normal stress, these four types of magma ascend edseparately and successively along the same channel way down ward, and finally were consolidated at the present place. In every time, the injected and intruded magma was emplaced on the lower side or on the roof of the former magma bodies. The good growth of the sulfide-rich and crystal olivine-bearing magma and its orebody-forming injection indicate the main metallogenetic stage and minerogenetic climax stage. The whole metallogenetic processes: deep seated magmatic liquid unmixing, crystalization of olivines and stratified action by gravity→the first stage silicate magma ascending→the second stage sulfide-bearing magma ascending→the third stage sulfide-rich magma injecting→late sulfide ore magma injecting→metasomatic min-erogenesis by contact→superimposed hydatogenesis, constitute an integrated minerogenetic model of copper nickle sulfide deposit and also a series of the temporal and spatial distribution
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