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The processing is useful when the source process is simple, for instance for a fixed point source or a unilateral rupture, but less effective in complicated rupture scenarios involving multiple simultaneous sources.
This relation depends on our interpretation of the source process.
This estimation, however, is based on our interpretation of the source process in region 1.
The power law model implies self-similarity of the source process.
The corresponding records should provide us with important information on the source process of this earthquake.
For example, Yagi et al. (2016) and Yamanaka (2016) estimated the source process using teleseismic records.
The source process of the 2004 Sumatra earthquake was estimated from teleseismic, tsunami and geodetic data.
Because of the uncertainty, the source process cannot be directly determined by the seismic source inversion.
The source process was estimated by the fully Bayesian multiple-time-window source inversion (Kubo et al. 2016).
The DSTF better describes the source process, whereas the direct solution of the waveform inversion is the FSTF.
The source process of the M 6.5 event (April 14, 2016, 21 26, JST) was also estimated.
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