Paishanlou Gold Deposit is hosted in Archean Jianping Group Dayingzi Formation metamorphic rocks and is controlled by near EW Donggou-Majiahuang ductile-shear zone.The main ore bodies T1,T8 and T4 are influenced by thrust nappe structure.The T4 is located in the north,the T1 is in the middle and the T8 is in the south.T1,T8 and T4 don’t pinch out in the strike or vertically,conforming to the lithological sequence of wall rocks which is dolomitic mylonite-ore body-biotite anorthosite mylonite and felsic mylonite.It is considered that there are potentials in the strike and deep part of T1,T8 and T4 ore bodies.Metallogenic predictions in the deep part are carried out,delineating 2 target areas.The verification in BQ2 target area turned out successful,indicating there are prospecting prospects in the deep part of Paishanlou Gold District.