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As shown in Table 2, the errors are less than 9% in 10 km depth, 5.5% in 15 km depth and 4% in 20 km depth.
d Shear wave velocity at 2.3 km depth.
This region also has anomalously low shear-wave velocities down to 100 km depth.
Here, the décollement dip increases (> 3°) cutting through deeper sediments to reach 10 km depth.
In this study, we examined discrete slip zones at 1 4 km depth within a major thrust and at 2.5 5.5 km depth within an ancient megasplay fault.
In Fig. 7b (9 km depth) and c (15 km depth), many aftershocks surround the Needles fault, characterized by high positive stress changes of more than 6 MPa.
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Fig. 7. Temperature distribution at 24-km depth.
greater than 140-km depth, where resistivity was 10 Ohm.
The 1D model was composed of five layers: from 0- to 10-km depth, where resistivity was 1000 Ohm from 10- to 30-km depth, where resistivity was 10 Ohm from 30- to 40-km depth, where resistivity was 100 Ohm from 40- to 140-km depth, where resistivity was 1000 Ohm greater than 140-km depth, where resistivity was 10 Ohm.
MRI and JMA (2007) proposed a spherical source at a 0-km depth and a dike at a 2.5-km depth.
Based on the GNSS data, MRI and JMA (2007) proposed a spherical source at a 0-km depth and a dike at a 2.5-km depth.
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