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The southeastward dipping plane is the source fault plane.
Both viscoelastic structure models with and without the slab predict landward motion above the source fault and trenchward motion in a region far from the source fault.
In Model C, the Gifu-Ichinomiya segment is not included in the source fault model.
Black lines show the source fault of the 1891 Nobi earthquake.
The spatial extent of aftershocks is used to estimate the source fault location.
Specifically, similar aftershocks on the source fault are located outside of the asperity.
Furthermore, the precise location of aftershocks can suggest a rupture pattern on the source fault.
Blue line represents surface projection of source fault plane of foreshock.
The aftershock distribution of large earthquakes is essential for estimating the extent of a source fault.
This method assumes that the source fault of the EGF event is finite.
Table 3. Source fault parameters for the assumed characterized source model.
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