Integrated analyses of the Ordovician carbonate outcrops and downhole data in the Tarim Basin show that the strik-slip fault facies of the Ordovician carbonatic rock is of large variety. Based on the development degree of internal structures, faulting can be divided into two types: well-developed fault core and undeveloped fault core. Using seismic profiles, structural map and coherence data, the authors identified the characteristics and development degree of strike-slip fault facies in Ordovician carbonate. The characteristics of strike-slip fault facies and their control over the pools are of great significance for carbonate reservoir modeling exploration and development.