The Shuangwang gold deposit, located in the east of the Fengtai ore concentration area of West Qinling, is a large gold deposit of auriferous albite breccias type. The ore deposit occurs in the weakly metamorphosed upper Devonian Xinghongpu Group, dominated by calcareous siltstone, sericite silty slate and carbonate that comprise flyschoid formation.Gold mineralization is strictly controlled by auriferous breccia bodies. Pyrite is the most important ore sulfide, and the main wall-rock alteration is albitization. Based on the regional geological-structural background, it is concluded that the mineralization of the Shuangwang gold deposit was related to the Late Triassic collision between the North China Plate and the Yangtze Plate. The Shuangwang gold deposit is genetically a cryptoexplosive breccia type gold deposit.