The　Zijinshan　Mining　Field,　which　is　dominated　by　the　Zijin　copper-gold　deposit,　is　the　first　highsulfide　epithermal　deposit　discovered　in　China.　The　porphyry　copper　(molydenum)　deposit,the　meso-lowtemperature　hydrothermal　copper　deposit,　the　lower-　sulfide　epithermal　silver　(gold-copper)　deposit,　the　volcanic　uranium　deposit　and　the　high-temperature　hydrothermal　tungsten　(tin)　geochemistry　abnormity　were　discovered　in　the　depth　and　vicinity　of　the　deposit.　From　late　Jurassic,　it　had　gone　through　multiphase-tectonic　movement,　magmation　and　hydrothermal　alteration,　which　had　resulted　in　multiphasemineralization.　This　paper　points　out　that　the　mineralization　system　of　the　Zijinshan　Mining　Field　is　characterized　by　tectonic　structure,body　within　body,altered　alteration,mineralized　mineralization,　and　by　a　vertical　zonation　of　minerlization:　＂U.,Ag-»＇Au-»-Au,Cu-*＂Cu-*-Cu,　Mo-*-W.wSn＂　from　top　to　bottom,　and　a　＂multi-storey＂　metallogenic　model.　The　different　deposit　types　show　laterally-distributed　patterns　spatially,　forming　a　unique　Zijin-typed　metallogenic　series　and　minerization.　Compared　with　other　deposits,　it　is　likely　that　the　porphyry　copper　(　molydenum　)　deposit　and　the　high-temperature　hydrothermal　tungsten(tin)　may　exist　at　the　depth　of　the　porphyry　copper　(molydenum)　deposit　and　its　vicinity　respectively.　The　research　shows　that　there　will　be　a　new　exploration　field　in　the　mining　field　and　provides　a　scientific　base　for　further　exploration.