Fig. 4.
From: Conceptual multi-scale dynamic rupture model for the 2011 off the Pacific coast of Tohoku Earthquake
Source time function normalized by total seismic moment for each model. Model B2 represents the same condition as Model B, except for a stress excess of 5 MPa instead of 6 MPa. The magnitudes obtained are all 8.5 except for Model B for which it is 8.6. For reference, the broken line represents the trend obtained by kinematic teleseismic inversion of the Tohoku Earthquake (Ide et al., 2011).