The ijinshan orefield ,a high- sulfide equithermal deposit discovered at first in China,is primary composed by Zijin copper-gold.The porphyry copper (molydenum) deposit,the meso-low-temperature 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 its depth and vicinity. From late Jurassic era,it had gone through multiphase-tectonic movement ,multiphase-magmation and mulaiphase-hydrothermal alteration ,and which had resulted in multiphase-mineralization. In this case, this paper points out that the Zijinshan orefield`s various tectonics-fluids-mineralization system is characterized by tectonic structure,body in body,alteded alteration,mineralized mineralization,and it possesses a spatial distribution of deposits characterized by minerlization vertical zoning features, “U、Ag→Au→Au、Cu→Cu→Cu、Mo→W、Sn”and “multi-floor building “ forming deposits modle. The vary metallogenic deposits appear unique distributing pattern, thus constitutes “Zijinshan” metallogenic series and metallogenic modle. Compare with other deposits,the porphyry copper (molydenum) deposit below copper-gold deposit and the high-temperature hydrothermal tungsten(tin) at its vicinity are cognitioned It indicates the new spatiotemporal field in discovering such ore type.,and offeres evidence for further prospecting