Fig. 4.From: A dynamic model of the frequency-dependent rupture process of the 2011 Tohoku-Oki earthquake(a) Low-pass filtered (<0.1 Hz) and high-pass filtered (0.5–1.0 Hz and >0.75 Hz) peak slip rates as a function of distance to the hypocenter. (b) Calculated power of the high-pass filtered peak slip rates. (Color figure is in online version.)Back to article page