Abstract: Taili Gold Deposit is located in the east of Shanhaiguan paleo uplift of Yanshan subsidence zone of North China Plate,and is a newly found deposit in the south end of Fuxin-Taili ductile shear gold metallogenic belt.The ore(mineralization)body of Taili Gold Deposit occurs in the Archaean granitic gneiss and is distributed along the secondary brittle fracture of ductile shear zone and is evidently controlled by ductile shear zone,possessing the feature of multiphase and multistage metallogenesis.The final oreforming period is the middle and late Yanshanian.The deposit genesis belongs to Archaean green stone construction post ductile shear zone fractured alteration rock type gold deposit.