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From this fault tree analysis is used to evaluate a pressure control system.
The initial uplift of the sea surface from this fault model is shown in Additional file 3: Figure S3.
Seafloor displacement from this fault is small, indicating that either recent sedimentation has obscured any surface offsets or the fault currently is inactive.
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This will give indication about the determination of the intersect point and its expected depth according to AB/2 is very important for forward modeling and in determining the depth to the peak either shallow or deep for this fault from the surface.
Numerical simulations for a dynamic rupture propagation from this buried fault (Fukuyama and Mikumo, 2006), and a point source model using historical seismograms (Fukuyama et al., 2007), have also been suggested.
This fault extends from the toe of the source area to near the crown.
Many reasons have been advanced to justify this departure from the fault principle.
Specifically, we show that there exists a nonattenuating stress field behind the Mach front that radiates high stresses arbitrarily far from the fault (practically this would be limited to distances comparable to the depth of the seismogenic zone), thus being capable of creating fresh damage or inducing Coulomb failure in known structures at large distances away from the main fault.
If there is any warping deformation away from the fault trace, this method would underestimate the total slip.
Laboratory experiments on rock samples from the fault show that this spectrum of slip behaviours is a natural consequence of shearing at slow plate-convergence rates.
This shows that as distance from the fault decrease, the probability of landslide occurrence increases.
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