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The source region extends along the Sagami trough from the Miura peninsula to the offing of the southern Boso peninsula, which covers the southern two thirds of the source region of the 1923 Kanto earthquake.
The type of clay found in a given area is a function of the source region on land and the climate.
Our OBS network is located at the southernmost region of the source region.
The solar B0 angle also affects the latitudinal distance of the source region from the ecliptic.
The locations of the source region and Kyushu island are shown in the inset.
This indicates the inhomogeneity of the source region together with variable melting of the source.
Acoustic modes are limited in the vicinity of the source region due to these characteristics.
A relatively large afterslip is estimated in the south of the source region.
In particular, we calculated the stress distribution numerically using a 3D crustal structure model of the source region.
Fig. 6 Test results for inversion uncertainties and the effect of the source region on the PHS slab.
The range offset analysis succeeded in mapping the ground displacement in the proximity of the source region (Figure 2a).
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