The Dushanzi anticline locats in the west segment of the southern margin of the Junggar Basin, it is a fault-related fold which developed by the thrusting of the northern Tianshan. Based on a seismic cross-section across the Dushen 1 well, the authors build the reasonable geometric model of the Dushanzi anticline by the well data and outcrop data. The results show that the Dushanzi anticline is a Trishear fault propagation fold, it developed in the Quaternary in the late Himalayan with a average thrusting slip rate 0.18 mm/a, then the structural deformation reached to a maximum thrusting rate in the Holocene with a slip rate 4.64 mm/a. The Dushanzi anticline has a total displacement slip more than 5 600 m, so it‘s average thrusting rate in the Quaternary is about 0.19 mm/a.