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On the other hand, interplate aftershocks occurred in the northern, southern, and deeper extensions of the large coseismic slip area.
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Seismicity around the segment is low, and that in the deeper extension is high.
These results suggest that the tremors occurred near the deeper extension of the Hinagu fault zone.
The relocated events are in good correlation with the estimated deeper extension of the active faults in the area.
The aftershock plane coincides with the deeper extension of the range-bounding fault estimated by Abe et al. (2008).
A deeper extension of the Dedana fault can be recognized on the seismic reflection profile (Abe et al., 2008).
This boundary coincides with the deeper extension of the Hakushu fault of the ISTL fault system, which has not produced a major event for more than 6,500 years.
These observations suggest that the tremors were triggered at the deeper extension of the active fault zone under stress conditions similar to those in the shallower seismogenic region.
Iio et al. (2004) proposed a model indicating that slip on a deeper extension of an active fault is required to generate large intraplate earthquakes.
On the basis of GPS measurements, Ohta et al. (2008) revealed that no coseismic slip was estimated at the deeper extension of the Dedana fault.
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