| Autor: |
Hisahiko Kubo, Iwaki, Asako, Suzuki, Wataru, Aoi, Shin, Sekiguchi, Haruko |
| Rok vydání: |
2019 |
| DOI: |
10.6084/m9.figshare.9877175 |
| Popis: |
Additional file 1: Figure S1. Planar projection of the total slip distribution. The slip contour interval is 0.8 m. The vectors denote the direction and amount of slip of the hanging wall side. The open star denotes the rupture starting point. Figure S2. Slip-velocity time function of each subfault. The star denotes the subfault corresponding to the rupture starting subfault. Figure S3. Maps showing some selected layers of the J-SHIS v2 3D velocity model. The triangles denote K-NET and KiK-net stations shown in the forward waveform simulation (Figs. 4 and 5). (a) Depth of the bedrock (VS = 2900 m/s), which reaches a depth of approximately 10 km west of the Hidaka Mountains. (b) Bottom interfaces of two selected low-velocity layers (VS = 700 m/s and 1100 m/s) of Late Miocene to Pliocene, distributed in a north–south direction west of the Hidaka Mountains and the source fault. Figure S4. Comparison between observed (black) and simulated waveforms (red) in the forward ground motion simulation for the aftershock (MJMA 5.4) at 6:11 JST on September 6, 2018. The number on the left of each waveform denotes the maximum absolute amplitude in cm/s. Figure S5. Simulated PGV distribution for the aftershock (MJMA 5.4) at 6:11 JST on September 6, 2018. The PGV is the maximum absolute amplitude of the vector sum of the three-component velocity waveforms low-pass filtered at 0.5 Hz. The triangles denote the observed PGV at K-NET and KiK-net stations for comparison. |
| Databáze: |
OpenAIRE |
| Externí odkaz: |
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