摘要
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 related to copper and potassium alkaline submarine volcano complex, and magmatic activities provided hydrotherm and heat for gold mineralization. It is a typical of gold deposit association resulted from the Tongshi subvolcanic medium-low temperature hydrothermal metallogenic system. With each deposit as an independent unit in the united metallogenic model, they constitute a relatively complete metallogenic sub-series.