笔者通过对新疆喀拉通克一号铜镍矿床的深入研究，得出了一些新的认识，即该矿床按侵位顺序可划分为岩浆熔离型、深熔贯入型和热液叠加型等成矿作用，其中后二者与贵金属的富集及成矿关系最为密切，尤其是热液作用最明显，例如：通过分析研究发现，贵金属Au、Ag、Pt、Pd主要在热液成矿流体分异形成的高铜块状矿体中富集；含矿岩浆在岩浆房中深熔的时间与各成因类型矿体侵位是反序的；Cu、Ni及贵金属成矿是经深源熔离和脉动式多次成矿作用而形成的． Based on the in-depth study of the kalaitongke-1 copper-nickel deposit in Xinjiang, the author has come to some new understandings that the deposit can be divided into magmatic ebbing type, deep-melt penetrating type and hydrothermal superposition type For example, according to the analysis and research, it is found that the Au, Ag, Pt, Pd of precious metals are mainly deposited in hydrothermal mineralization Fluid rich in high copper lump ore body enrichment; ore-bearing magma in the magma room deep melting time and the genetic type of ore body emplacement is reverse order; Cu, Ni and precious metal mineralization by the deep source Melting and pulsation multiple mineralization formed.