Exact(1)
The maximum slip estimated using a sparsity constraint was comparable to other studies.
Similar(7)
The seismic moment and maximum slip were estimated as 5.5 × 1019 Nm (M w 7.1) and 3.8 m, respectively.
The major slip area is located around the asperities of the 1981 Miyagi-oki (M 7.2) and 2003 Fukushima-oki (M 6.8) earthquakes and the maximum slip is estimated as being up to 35 m.
c Standard deviation of slip estimated from Monte Carlo simulations.
The seismic moment and maximum slip of the estimated source model of the 2015 Gorkha earthquake are 7.5 × 1020 Nm (M w 7.9) and 7.3 m, respectively.
The estimated maximum slip is ~65 m, and the seismic moment estimated with the variable rigidities based on the layered velocity structure used for Green's function computation is ~4.2 × 1022 Nm (Mw 9.0).
According to the detailed slip distribution on the fault plane, the major slip area was south of the main shock in a shallow area and the estimated maximum slip is as large as 5 m. Figure 10 shows the comparison of V p perturbation distribution and location of large coseismic slip.
The estimated maximum slip was approximately 40%% less than the true value.
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