LA-ICP MS Zircon U-Pb dating results of granitoids from Sawuer Mountains in North Xinjiang, NW China, are reported based on 1:50 000 regional geologic survey. Zircon U-Pb dating shows that the granitoids have magmatic crystallization age of 320±2 Ma. The petrology and geochemistry of granitoids from Sawuer Mountains suggest their mixing origin. The granitoid from Sawuer Mountains occurred in an extensional setting, most probably related to post-orogenic processes during the closure of the Peo-Asian Ocean, namely, represent the tectonic setting shifted from typical continental arc to post-collisional setting.