The gold polymetallic deposits in the Weizigou area of Liaoning province are mainly controlled by fault structures.Limonite

pyrite

kaolinization and potashization are the main alteration features. The surrounding rocks are Cretaceous granites and New Archean missed granites. The exploration of metallogenic regularity in this area has been explored through soil geochemical measurements

induced polarization（IP） measurement

trench exploration engineering and drilling engineering. It is believed that the mineralization in this area is controlled mainly by fault structures and has obvious zonality.The formation of polymetallic mineralization is closely related to the Archean hybrid granite.