The Xiaohongshilizi silver lead-zinc deposit is occurred in volcanic dome structure setting, ore-control was related to the marine volcano-sedimentary formations. The hydrothermal alteration types have zonality and in metallic mineralization of ore body, and element distribution in space, demonstrated that the deposit belongs to volcanogenic-massive sulfide deposit in volcano dome structure environment. Speculate further, in the same central part-Jilin arc structure belt are Dijuzi, Xinlitun, Erdaolinzi, Quanling etc. On this basis, the authors put forward some prospecting and evaluation criteria of geosynclinals area massive sulfide polymetallic deposits within