Fig. 3.From: A dynamic model of the frequency-dependent rupture process of the 2011 Tohoku-Oki earthquake(a) Initial shear stress, static strength and dynamic strength in the numerical model set-up as a function of distance to the hypocenter. (b) Spatiotemporal distribution of slip rate. (c) Peak slip as a function of distance to the hypocenter. (Color figure is in online version.)Back to article page