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SMGA can be divided into (N times N) equivalent-sized subfaults with the same rupture area of the EGF event.
First, events within a multiplet were located within the same rupture zone which showed that the same asperity was reloaded and broken several times during the injection period.
Thus, if we assume that the slip deficit has accumulated for 200 or 300 years, it would create a twofold or threefold amount of slip in the same rupture area.
We consider multi-hypocenter; that is, when the rupture front reaches a point within an asperity, the rupture is assumed to propagate within the asperity from that point with the same rupture velocity but with new wave fronts.
Also, accurate P- and S-wave differential arrival times between events were obtained by applying waveform cross-correlation in the time domain to minimize the errors, by an order of magnitude or more, in the case of earthquake pairs having the same rupture mechanism and a similar waveform (Schaff and Waldhauser, 2005).
Similar(55)
For multi-segment ruptures, researchers have discussed whether or not the repetition of the same dislocation rupture characterizes each of the segments of a long active-fault zone (e.g., Sieh, 1996; McGill and Rubin, 1999; Kaneda and Okada, 2008).
Our result appears to be consistent with their result in that it has no repetition of the same dislocation rupture for the Neodani segment.
The above described model shows one and the same the rupture origin and universal mechanism could be considered in its frames.
The repetition of the same dislocation rupture for each segment is not considered in existing construction methodologies for the characterized source model for strong ground-motion prediction, such as the methodology developed by HERP (2008b).
The same section ruptured again and increased the offset amount during the mainshock that produced the 31-km-long surface rupture along the central to northeastern part of the FHFZ.
The same type ruptures had been observed in a delta located in Gölcük-Kavaklı Gölcük-Kavaklırnearulthend of the 1999 Kocaeli (Turkey) earthquake, and westernined as the Kavaklı normal fault (Barka endal., 2002).
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