Results of dislocation modeling of the Kawabata sedimentary basin. (a) Simulation based on a simple compressive regime. (b) Compressive model based on unrealistic fault distribution. (c) Simulation based on a transpressional regime assuming propagation of fault terminations. Names of fault abbreviations and optimized fault parameters are given in Table 2. Fault names adopted for numerical modeling are after Kusumoto et al. (2013).