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To construct the heterogeneous source models (Models H1, H2, and H3), multi-scale heterogeneity was cumulatively added to the spatial distributions of the slip D, rupture velocity (V_{text{R}}), and rake angle (lambda), using Model C as the initial model.
We have previously proposed multi-scale heterogeneity in fracture energy using circular patches of different sizes on the fault plane.
Moreover, the radiation of ground motion based on this multi-scale heterogeneity has not yet been discussed.
Then, multi-scale heterogeneity was added to the spatial distribution of several source parameters to yield a heterogeneous source model.
First, multi-scale heterogeneity is added to the spatial distribution of slip in Model C to yield Model H1.
We present conceptual dynamic rupture models for the 2011 Tohoku Earthquake based on multi-scale heterogeneity in fracture energy.
We address them below in the context of multi-scale heterogeneity on which the present simulations are based.
The main effect of the multi-scale heterogeneity in Dc is on the rupture velocity, as well as the rupture directivity (Ide and Aochi 2013).
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