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The seismic moment and maximum slip were estimated as 5.5 × 1019 Nm (M w 7.1) and 3.8 m, respectively.
Rupture velocity and maximum slip were left relatively unconstrained (Vr = 1.25 3.25 km/s; maximum slip = 100 m), and moment minimization constraints were reduced, such that moment is controlled by the inverted data rather than by an assumed initial condition.
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The average slip (relative motion) between the two plates during the earthquake was approximately 5 m (16 ft), and the maximum slip was approximately 20 m (66 ft).
The maximum slip is about 28 m if the rigidity is assumed to be 30 GPa.
The maximum slip is found to occur deeper than the epicenter (143.3, 38.3) (JMA, 2011).
The maximum slip is larger in the regional analysis because of a spatially finer resolution.
The estimated maximum slip was approximately 40%% less than the true value.
The maximum slip is about 24 m for case 300_3 and 20 m for case 400_5.
The estimated seismic moment and maximum slip are 7.5 × 1020 Nm (M w 7.9) and 7.3 m, respectively.
The seismic moment and maximum slip are 5.5 × 1019 Nm (M w 7.1) and 3.8 m, respectively.
For the series tested by Abtan, the calculated values of maximum slip are reasonably close to those observed by experiments.
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