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Fig. 5 Snapshot of the rupture process.
(c) The rupture time-distance relationship during the rupture process.
The effect of rupture process on near-source ground motions .
Synthetics calculated from the estimated rupture process are compared with the observed data in Fig. 5.
Next, we perform a joint inversion for the rupture process and assume the rupture velocity.
Near-field waveforms are most effective to investigate the spatiotemporal earthquake rupture process.
These conditions prevent conventional back-projection analysis to reveal the details of the rupture process.
However, these studies did not properly consider the dynamic rupture process of the 2011 Tohoku earthquake.
The rupture process of the Tohoku earthquake has also been investigated by many researchers.
Thus, this slip might be an artifact of the main shock rupture process.
The simulated rupture process is consistent with Ide et al. (2011).
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