There are many shear zones formed in the process of formation and evolution of the Tongbai orogenic belt. This article focuses on the Dahe-Guxian shear zone and Yindian-Malong shear zone and analyzes their structural deformation characteristics, and uses mathematical method and graphical method to calculate displacement of the two ductile shear zones. The activities age of the Yindian-Malong shear zone is obtained by ESR dating of syntectonic quartz veins. The results are in good consistent with previous research in this area. The Dahe-Guxian shear zone has dextral shear sense and with displacement of 857~867 m. Its kinematic vorticity Wk is significantly greater than 0.75, which indicates a simple shearing. The Yindian-Malong shear zone also has dextral shear sense with displacement of 1 081~1 113 m, the quartz ESR dating results of 140.6~131.5 Ma, show that after Tongbai orogenic belt collision, the main tectonic deformation is shear activity, occurred in the Early Cretaceous period.