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So far three main genetic types of nickel deposit have been recognized in China:magmaticcopper-nickel sulfide deposits,nickel deposits occurring in the crust of weathering,and sedi-mentary nickel deposits.On the basis of the geotectonic settings of intrusive bodies,their gene-tic types,and the way sulfides are concentrated,the copper-nickel sulfide deposits fall into twobroad categories:deposits emplaced along paleolandmass edges and those in the mobile zones onthe outside of paleolandmasses.They can further be divided into six sub-categories and then avariety of types.The magmatic copper-nickel sulfide deposits constitute one of the most important genetic typesin China.Geological evidence shows that the individual ferruginous ultrabasic bodies intrudingalong paleolandmass edges are most favourable for Ni-mineralization.In the light of the paleo-structural analysis,the author has proposed three mechanisms withrespect to the formation of Ni-bearing ultrabasic bodies.
So far three main genetic types of nickel deposit have been recognized in China: magmaticcopper-nickel sulfide deposits, nickel deposits occurring in the crust of weathering, and sedi-mentary nickel deposits. On the basis of the geotectonic settings of intrusive bodies, their gene -tic types, and the way sulfides are concentrated, the copper-nickel sulfide deposits fall into twobroad categories: deposits emplaced along paleolandmass edges and those in the mobile zones on the outside of paleolandmasses. They can further be divided into six sub-categories and then avariety of types. the magmatic copper-nickel sulfide deposits constitute one of the most important genetic types in China. Geological evidence shows that the individual ferruginous ultrabasic bodies intrudingalong paleolandmass edges are most favourable for Ni-mineralization. the light of the paleo-structural analysis , the author has proposed three mechanisms withrespect to the formation of Ni-bearing ultrabasic bodies.