According to the spatial and original relationship between current hydrothermal metal deposits and magmatic body, and referring to the ideal mode of deposit element zone which is proposed first by Russian geochemist, this paper puts forward the ideal mode of the distribution of the magma hydrothermal deposits, which is also called “ore-forming system around magmatic rock center”. This mode is centered on the top rock mass which intrudes to the near-surface surrounding rocks, and it is divided into inner-zone, transition-zone, medium-zone and outer-zone. The mode scatters by hypothermal deposits, mesothermal deposits and epithermal deposits from inner-zone to outer-zone regularly.