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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)).
Likewise, for the second wave group, the final slip distribution is only significant in the model with a free surface.
As a result, it was confirmed that the final slip distribution was not significantly affected by this modification.
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These factors result in an underestimation of the final slips in the shallower region compared to the inversion results.
Figure 2 shows the final-slip distribution.
Fig. 2 Map projection of the final-slip distribution.
Figure 9a shows the final-slip uncertainty of our source model.
Broken contours indicate the final-slip distribution with a 1.46-m interval.
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