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The rupture duration at each point is shown in color.
The assumed rupture duration was taken as 18 s.
The total rupture duration is approximately 5 s.
The rupture duration is assumed to be sixty seconds.
The total rupture duration is longer than LL events on average, and there is larger variation.
This is justified when the tsunami propagation distance over the rupture duration is much smaller than horizontal scales of interest.
Similar(28)
Slow slip events (SSEs), which are geodetically slow earthquakes with rupture durations of approximately one month, have been detected in the southern Ryukyu Trench.
Each subfault has a source time function parameterized by seven 8 s wide symmetric triangles, offset by 4 s each, yielding 32 s long subfault rupture durations.
Very low frequency earthquakes (VLFEs), which are categorized as seismically slow earthquakes with rupture durations of tens of seconds, occur along the trench axis (Asano et al. 2015; Nakamura and Sunagawa 2015).
(3) The rupture length, source duration, and rupture velocity of the northern segment were all larger than those of the southern segment.
The aforementioned results show that the rupture velocity of southward faulting is lower than that of northward faulting; furthermore, the rupture length and source duration in the southern fault are also shorter than those in the northern one.
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