The Jinlongshan gold deposit is located in the fold-and thrust belt of south Qinling orogenic belt and mainly hosted in the carbonate and clastic rocks. Mineralization is controlled by liernthology and the degree of ductile-brittle structural deformation. In terms of the geological-geochemical characteristics of the Jinlongshan gold deposit being similar to Carlin-type gold deposit, it can be classified to the class of Carlin-type gold deposit. The Jinlongshan gold deposit formed in the intracontinental subduction tectonic setting and was a result of intracontinental orogeny of Qinling orogenic belt.