Bengbu Uplift Area is an important component section of North China Craton. However, it has been restricted for people to have a comprehensive understanding of how Bengbu Uplift Area formed and evolved due to the weakness of previous research on its metamorphic crystal basement and geochronological analysis. In this research, garnetbearing granitic gneisses of ZhudingShimen Mountain region in the east Bengbu Uplift Area will be studied in order to identify the metamorphic conditions and time limits of Wuhe group.Methods:In this study, detailed petrographic, mineralogical geochemistry analysis and LA-ICP-MS zircon U-Pb chronology have been conducted on garnetbearing granitic gneisses of Zhuding-Shimen Mountain region. Results:Their P—T conditions are T=736~788 ℃ and P=0.76~0.89GPa, which indicates that they formed under the lowpressure granulite facies condition. Zircon dating analysis has recorded the magmatic crystallization and metamorphism, for the time are 2562±34Ma ~ 2584±25Ma and 2433±31Ma ~ 2436±24Ma respectively.  Conclusions:This study analyzes the garnet-bearing granitic gneisses of Zhuding—Shimen Mountain region, so that the metamorphic conditions and time limits of Wuhe group have been identified. Meanwhile, it helps to complete the regional geological data and provides basis of basement attributes of Bengbu Uplift Area.