As a result, propagation slows, and there is more time for the lost-dome region to recover while the delayed-dome region is still capable of producing diffusive currents that bring the lost-dome region above the threshold of excitation, resulting in P2R.
They concluded that it was most plausible that these migration sequences were due to the propagation of slow slips.
This deceleration might be related to a diffusional propagation of slow slip as considered in the above-mentioned studies.
Propagation both slow magnetosonic wave and Alfven wave can easily be canalized along the magnetic field line direction.
Kato et al. (2012) interpreted the inter-plate foreshock migration before the 2011 Tohoku earthquake as propagation of slow slip.
Supported by these established observational facts, we can safely interpret the seismic activity change as the marker of the propagation of slow slip, i.e., after-slip.
Although propagation is slow (and will also be addressed in Section 2.4), it constitutes a zero-day attack and presents an attractive attack vector for potential attackers.
In most profiles, cracks also initiated at the sharp notch at the weld, but the propagation was slow and complete fracture never took place there.
However, for the propagation of slow mode, the following condition on the wave propagation angle θ should be satisfied θ > tan - 1 Z p + 2 σ p - v z 0 v x 0. (9)The above equation shows that there exists a minimum wave propagation angle ( θ min ) below which the slow mode does not propagate in the plasma.
Because the propagation of slow slip induces stress perturbation on and around plate interfaces, we can expect the occurrence of earthquakes that are triggered by slow slip in the current sequence, as has been observed along the currently targeted subduction zone (e.g., Miyazaki et al., 2004; Uchida et al., 2004).
