Jinqingding quartz-vein type gold deposit is located in the central area of Muping-Rushan metallogenic belt. Based on the structural mapping, the analysis of paleotectonic stress inversion and the differential paleostress values, the authors studied the tectonic movement features and tectonic evolution history preliminarily. The results show that the ore-controlling fault of this deposit has gone through three stages of activity, characterized by left-slip transgression before mineralization, right-slip extension transtension during mineralization and intrusion of lamprophyre, and left-slip transgression after mineralization.