Skip to main content


Figure 9 | Progress in Earth and Planetary Science

Figure 9

From: Mechanism of long-standing Cenozoic basin formation in central Hokkaido: an integrated basin study on an oblique convergent margin

Figure 9

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 TableĀ 2. Fault names adopted for numerical modeling are after Kusumoto et al. (2013).

Back to article page