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Fault dimensions of the faulty induction motors are described in Table 1.
N and C indicate the ratios of the fault dimensions and stress drops, respectively, between the target and the small events.
Their slip model has a grid spacing of 25/50 and 50 km and fault dimensions of 200 and 550 km in the down-dip and along-strike directions, respectively (Figure 1).
Another relevant aspect that needs attention in tsunami sensitivity analyses is the consideration of new scaling relationships for fault dimensions of mega-thrust subduction earthquakes (e.g. Murotani et al.2013).2013
Abe (1977) estimated the fault dimensions and dislocations of those interplate events of 1938, based on the aftershock distribution, tsunami source area, and forward modeling of regional long-period seismograms using the Haskell-type source model.
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The pattern of waves produced is dependent on several parameters, such as fault dimension and rupture velocity.
Since actual fault sizes of small earthquakes are unknown in most cases, we usually estimate the fault dimension from the observed corner frequency.
As the stress drop analysis from the observed corner frequencies usually assumes that the rupture speeds of earthquakes are the same, the fault dimension of earthquake X is overestimated, thus resulting in an estimated stress drop for earthquake X that is an order of magnitude smaller than the actual one and the value of earthquake Y.
For the second event at 22 43 UT, we defined the fault plane dimension to be 90 km in length by 40 km in width based on the scaling relation proposed by Murotani et al. (2008) and constraining the fault plane from intersecting the free surface.
The fault 3 fractal dimension is the largest.
We considered a large planar fault with a dimension of 500 km (along strike) by 200 km (along dip).
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