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The effect of the rupture with Britain and the liberal principles it represented was to push Louis-Philippe into closer alliance with the conservatives, led by Guizot, at a time when the liberals were gathering strength.
Figure 2(c) suggests that the effect of the rupture directivity is also an important consideration.
In the previous section, it was demonstrated that the rupture of the Yunodake fault was caused by the dynamic effect of the rupture of the Itozawa fault.
Time-dependent Coulomb failure function changes (ΔCFF) were calculated using the stress change from the Itozawa fault rupture in order to evaluate the effect of the rupture on the Yunodake fault.
Although this source model was estimated by considering the effect of the rupture process on the fault plane, we assume that the coseismic crustal deformation is immediately completed at time (t=0) in order to focus on the influence of the complexity of the fault model.
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Effects of the rupture were felt over an area of.
The effect of the fault rupture zone traversing a seismically isolated bridge is investigated utilizing a finite element model of a section of the Bolu Viaduct and a set of synthetic broadband strong ground motions simulated for the Bolu Viaduct site due to the 1999 Duzce earthquake.
Therefore, information about the effect of the earthquake rupture on the damaging ground motions in Mashiki could be obtained from including KMMH16 in the inversion analysis.
The velocity pulse and pulse-like ground motions observed near surface of the faults can be considered to be the effect of the forward rupture directivity or the tectonic offset (e.g., Loh et al. 2000; Mavroeidis and Papageorgiou 2003; Hisada and Bielak 2003; Baker 2007; Dreger et al. 2011).
Therefore, we consider it important to calculate the time-dependent ΔCFF using the obtained moment release history of the Itozawa fault in order to evaluate the effect of the Itozawa fault rupture on the Yunodake fault plane.
Furthermore, the obtained time-dependent ΔCFF was found to be larger than the static ΔCFF caused by the 2011 Tohoku earthquake, which implies that the effect of the Itozawa fault rupture on the Yunodake fault plane was larger than that of the 2011 Tohoku earthquake.
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