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Few fore- and aftershocks occurred in the large slip areas.
Area 1 includes the large slip area near the hypocenter, and Area 2 includes the shallow large slip area north-northeast of the hypocenter (Fig. 8a).
Z-shaped hysteretic curves reveal the large slip of the joint with the cover plates.
High-frequency waves were mostly produced at small asperities surrounding large slip areas.
The contribution of the large slip region to the seismic waveforms was significant at many stations.
Seafloor geodetic observations also provide evidence for a large slip (Sato et al., 2011).
Whether the SMGAs coincide with the asperity areas of large slip is discussed below.
A striking feature is the large slip in the shallower region.
One possible cause of the underestimation is the shallow large slip that causes fling steps.
The occurrence of such a large slip implies a large stress drop associated with the earthquake.
The large slip near trench is not common for great (Mw > 8) subduction earthquakes.
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