Huangshaping Pb-Zn polymetallic deposit is hosted in contact zone between the Lower Carboniferous Shidengzi Formation carbonate and Yanshanian acid intrusive rocks. The ore-bodies are controlled by strati- graphic occurrence, teetonic-magmatic activity and wallrock alteration. The ore-type, ore-body fabric and wall rock alteration types with obvious banding features are closely related to contact zone, tectonic and stratigraphic distribution. An extra large W-Mo-Bi-Sn polymetallic deposit is found in deep and edge of Huangshaping large lead-zinc deposit based on metallogenic regularity research.