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- W2605518069 abstract "We simulate dynamic mode II rupture that finally forms a branched fault trace, where our main interest lies in the resultant seismic wave radiation due to the dynamic branching process. For this purpose we adopt the elastodynamic boundary integral equation method, which enables us to work with non-planar fault geometry. We consider a medium under biaxial compressional load in which Coulomb friction acts on rupture surfaces and apply a critical shear stress criterion in determining the direction and the extension of rupture tips. In our simulation, dynamic branching first occurs due to local off-plane stressing around the fast propagating tips and each branch increases its bending angle. The stress to be released on such branch becomes negative under biaxial compression, the growth of each branch is thus arrested spontaneously. In order to find phases associated with the dynamic branching process, we synthesize waveforms of the branching model and compare them with those radiated from a planar fault model whose growth is arrested without branching. When the observation point is very near the branching point, we can successfully identify a distinct branching phase in a component for which no wave radiation is expected from the planar model. Otherwise we can not find significant effect of the dynamic branching process on the seismic wave radiation: this is because the moment release rate on the branching part of the fault is negligible compared with that on the entire fault." @default.
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- W2605518069 date "2005-01-01" @default.
- W2605518069 modified "2023-10-18" @default.
- W2605518069 title "Seismic Wave Radiation of Dynamic Rupture in Branched Fault Modeling" @default.
- W2605518069 doi "https://doi.org/10.4294/zisin1948.57.3_377" @default.
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