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We suggest that the lack of clear normal faults in the reflection image is precisely because our seismic profile is oriented almost orthogonal to the arc strike (i.e., extensional direction) and is thus sub-parallel to the strike of normal faults.
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Latest approaches also consider the issue of multiple faults in reflection to the characteristics of modern day systems designed for high reliability.
This indicates that the stress state lies in either a normal or strike-slip faulting regime throughout the section, which is broadly consistent with observations of abundant normal faults in the Kumano basin in seismic reflection data (e.g., Sacks et al. 2013) and with previous estimates of stress magnitudes from wellbore breakouts (Chang et al. 2010).
Seismic reflection profiles reveal steeply landward-dipping splay faults in the segments B and C. The splay faults, branching upward from the plate-boundary interface, almost reach the seafloor, producing the seafloor fault scarps.
Faults were imaged as high-attenuation stripes, demonstrating that SAP may contribute to detection of faults in the igneous section of oceanic crust where faults are rarely imaged by conventional seismic reflection methods.
The newly shown fault lines are among an estimated 15,000 faults in the state.
This function models k sequential faults in the network.
If n faults in the network exist then at most n faults can lie on any trajectoy.
Under the single-fault model, if the faults in the network are represented by a Boolean vector Δ of size N, at most one gene x i has a fault (i.e. Δ i = 1 for at most 1 bit).
In [ 3], the authors proposed modeling cancer as faults in the signaling network and applied fault analysis for drug intervention to control the GRN.
Robustness of attractors is measured as the number of faults in the network are increased from 0 (i.e. no stochasticity) to 5 faults.
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