Abstract: The collisional tectonic kinematics is one of the important studying methods of plate tectonics and is used to ascertain the senses of movement, the polyphase deformation and the tectonic evolution. The present authors have been working for more than l0 years in the jiangnan Proterozoic orogenic belt and the Eastern Tianshan Paleozoic orogenic belt and have obtained a plenty of in formation of ductile shear deformation and firsthand kinematic evidence. The authors presented and summaried the following research results of collision tectonic kinematics. 1. There are 6 geological indicators of the plate collision-suture zone, i. e., ① the tectonic melange, ② the high pressure metamorphic zone and region metamorphic zone, ③ the collision type granite, ④ the large-scale ductile shear zone, ⑤ the polyphase deformation zone and ⑥ geophysically abnormal zone. 2. The 4 major aspects for the research on lower and middle-deep seated tectonic kinematics are: ① the mylonitic rocks including feldspar-quartz mylonites, mylonitized rocks and phyllonites, ② special folding style such as sheath fold and recumbent fold, ③ stretching lineation, foliation and cleavage, ④ kinematic ductile shearing sense indicators including strain indicators, rotation indicators,shear indicators,etc. . 3. The 5 types of ductile shear zone are divided based on origin mechanism；① subduction type, ② thrust type, ③ fault zone type, ④ strike slip type and ⑤ extension type. Finally, the authors reported in brief some new results and understanding about the collision kinematics in the Jiangnan orogenic belt and the Eastern Tlanshan orogenic belt, for example, regional sense of shear and polyphase deformation (thrust, strike-slip and extension) corresponding to the evolution history of regional tectonics .