Geological structural features of the Agnie-Afanasyevsky deposit in the Lower Priamurye

The author considers geological structure of the Agnie-Afanasevsky deposit in the Lower Priamurye. It is determined that the gold-quartz veins are controlled by the S-shaped flexure, formed by terrigenous rocks of the Lower Cretaceous because of the 500 m amplitude left up-and-up shift along the northeastern fault. The flexure has geological and structural features, which are favorable for the new gold ore veins and stockwork ore bodies.