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Exact(8)
The maximum slip area of the 2011 Tohoku-Oki earthquake is located along MY102.
The source inversion result shows that the maximum slip area of the M7.3 event was close to this location (Kubo et al. 2016).
Therefore, there is an apparent contradiction between their results and our results that show a strong patch in the maximum slip area of the 2011 Tohoku-Oki earthquake.
The center of the maximum slip area was stable even when we have assumed various maximum rupture front velocities (Additional file 1: Figure A3).
We performed inversions using several dip angles and found that the center of the maximum slip area was stable (Additional file 1: Figure A2).
The profile of MY102 crossing the maximum slip area of the 2011 Tohoku-Oki earthquake presents a relatively large taper angle with high μ b ′ (approximately 0.26) and low λ (approximately 0.63) values.
Similar(52)
The shape of the large slip area is similar in both analyses, but the points at the maximum slipped area near the trench differ somewhat (about 50 km).
The area of maximum slip, with a value of ~5.7 m, was centered ~10 km northeast of the epicenter.
A large-slip (> 4 m) area with the maximum slip was found north of Kathmandu (from 60 to 100 km east-southeast of the hypocenter).
In our model of the Tokai SSE, the maximum pressure loss by 2009 in the slip area is about 300 MPa (Fig. 9).
The derived source model has a unilateral rupture toward the east and a large-slip area north of Kathmandu with the maximum slip.
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