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"Those are enormous slips," Wald says, running about two to three times the maximum slip reported for the magnitude-8.8 Maule, Chile, quake of last year.
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The majority of mothers who brought referral slips reported that they were attended to promptly (78%).
These studies reported the maximum slip amount was 4 6 m.
Seno and Hirata ([2007]) reported that the maximum slip of the tsunami models (approximately 30 m; e.g., Hirata et al. [2006]; Tanioka et al. [2006]; Fujii and Satake [2007]) is generally larger than that of the seismological models (approximately 15 m; e.g., Ammon et al. [2005]; Ji [2005]; Yamanaka [2005]).
Previous studies reported that the location of the maximum slip of the coseis-mic and postseismic areas is not in the same place.
The differences found in the stress field along the interface, maximum load, maximum slip, ultimate slip, fracture energy and effective bond length are reported.
For example, the maximum slip along the Nojima fault in our model is less than that reported by Yoshida et al. (1996) by about 0.3 m.
This model is based on three parameters: maximum bond stress, slip at maximum bond stress, and maximum slip.
The average slip (relative motion) between the two plates during the earthquake was approximately 5 m (16 ft), and the maximum slip was approximately 20 m (66 ft).
The results of the numerical simulation included slip values along the interfaces, maximum slip values, stresses and strains and deflections.
The maximum slip amount is 38 m.
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