摘要
///Yangshuqu, a recent found superlarge Au-Ag-Pb-Zn deposit, is located in the east Liaoning rift mineralizing belt. Mineralization is shallow buried, large scale and huge economic. Four main mineralizing belts are distributed in carbonate rocks interlayer with of Liaohe Group Dashiqiao Formation calyrocks and silicalite. Orebodies, consistent occurrence with the strata, exists as layer, stratabound and bean pod. Based on analyses on ore geology, geochemistry, isotope and mineralization mechanism, it is proven that the deposit is related obviously with volcanism and hot brine sediments overlaid intensively by late metamorphic and magmatic fluids.