The Fe deposit belongs to the effusion type (or volcanic deposition reformation type) related with Middle Triassic intermediate- acid volcanic rock in genesis. The Pb-Zn multimetallic deposit is related to Shanglan Formation slate, silty slate with intercalation of limestone, marl and Sanhedong Formation limestone in genesis, which is a Cu -Pb -Zn multimetallic deposit of hydrothermal type controlled by both strata and structure.