Fig. 7From: Dip angles of active faults from the surface to the seismogenic zone inferred from a 2D numerical analysis of visco-elasto-plastic models: a case study for the Osaka PlainResults for the numerical simulations without any preexisting fault zone. The newly formed faults (markers with a cumulative strain larger than 1) are illustrated in dark blue. a Case with the random seed number = 1. b Case with the random seed number = 3Back to article page