Gold mineralization type in the Guilaizhuang gold field are mainly composed of cryptoexplosive breccia rock type, magnesium carbonate microdisseminated type, skarnstacking type, porphyry and altered rock type and other types gold deposits (prospect). Its genesis is closely relted to copper and potassium alkaline submarine volcano complex, and magmatic activities provided hydrotherm and heat for gold mineralization. Subvolcanic dome consisting of complex and associated circular radial structures controls the distribution of gold ore bodis. NeoArchean Taishan Group is the main ore source bed; carbonate rock in the upper part of limestone member in the Cambrian Zhushadong Formation is favorable orebearing strata; dolomitic limestone and dolomite in upper Cambrian or lower Ordovician are favorable country rocks of the Guilaizhuang gold deposit. Gold(copper, iron) mineralization subseries related to metaalkalescence subvolcanic complex in the early Mesozoic Yanshanian also occurred in this area. Controlled by the subvolcanic dome, the orebodies occur in different geological bodies at various geological sections with various depths. It is a typical of gold deposit association resulted from the Tongshi subvolcanic mediumlow temperature hydthermal metallogenic system. With each deposit as an independent unit in the united metallogenic model, they constitute a relatively complete metallogenic subseries.