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Circles indicate that a rupture propagated successfully.
Triangles indicate that a rupture was initiated but terminated shortly.
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Hence, it indicates that a different rupture by another fault is necessary.
The clearest offsets indicate that the rupture broke a 270 km-long major segment of the Beichuan Fault and a 70 km-long segment of the Guanxian Fault, both trending ∼N55E.
Crosses indicate that no rupture was initiated.
The data also indicate that the rupture also occurred on the eastern extension of the Futagawa fault zone.
Therefore, we consider this to indicate that the rupture of the Yunodake fault was triggered primarily by the rupture of the Itozawa fault.
Our results indicate that the rupture occurred in both shallow and deep parts of the Nicobar region (areas B and C); this result was further obtained by Lorito et al. ([2010]).
Seismological and geodetic inversion models indicate that coseismic rupture not only occurred on shallow crustal faults but also at the Hikurangi subduction interface with small-scale thrusting-dominated movements (Hamling et al. 2017; Holden et al. 2017).
Thus, these observations clearly indicate that the rupture of the M 7.3 event occurred on multiple fault planes along the Hinagu fault zone, the Futagawa fault zone, and its eastern extension.
The cascade model indicates that a behavioral segment ruptures independently or along with other contiguous segments and assumes that repetition of the same slip at given point characterizes the behavioral segment.
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