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These factors result in an underestimation of the final slips in the shallower region compared to the inversion results.
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Finally, the directions of the final slip are shown in Fig. 13.
Contours are drawn every 2 m of the final slip.
Fig. 2. Projection of the final slip distribution on the map.
The final slip tapers almost linearly towards the bottom of the seismogenic zone (Fig. 3(c)).
Note that the dependence of the final slip distribution on the selection of the EGF events is small.
Likewise, for the second wave group, the final slip distribution is only significant in the model with a free surface.
Figure 9 shows the final slip distribution for the 2016 Kumamoto earthquake obtained from the waveform inversion Cases 1 4.
The final slip distributions for the foreshock and mainshock were compared with the spatial distributions of the aftershocks.
As a result, it was confirmed that the final slip distribution was not significantly affected by this modification.
The final slip amplitude is (U_{mathrm{a}} =0.05) and the geodetic moment is (M_{mathrm{a}}/M_1=0.10).
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