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An analytical solution is first developed for a simplified system subjected to continuous slipping motions.
This "ego," while its definition is modified over the course of Husserl's work, is characterized by the passive synthesis of time's unity and flow (as continuous slipping back of events, whose position in lived time remains determinable).
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This "continuous" slip through several grains was associated with the presence of a significant number of "low-angle" grain boundaries.
An additional experiment was performed under a continuous slip ratio from 0.2 to 0.6 with a wheel load of 50 N to validate the method.
Using the Peierls concept, a dislocation can be described by a continuous slip field, and the dislocation nucleation occurs when the total potential energy reaches a stationary state.
The large continuous slip patches may facilitate near-complete stress drop.
Lay et al. (2012) found decreased high-frequency radiated energy in zone B, suggesting large patches of continuous slip.
The longer period results may be representative of the continuous slip which seems to be dominated by one area of large slip.
By combining our methods with appropriate hyperparameter selection, it is possible to obtain a smooth distribution at a continuous slip area, and a discontinuous distribution at boundaries between non-zero-slip and zero-slip areas.
However, as shown in Fig. 1, this study's analysis estimated a continuous slip distribution over the whole source region, including the northern part, even when data in Naos Island were used.
Strongly coupled regions are termed asperity, which ultimately released seismic energy through large megathrust earthquakes due to slip concentration, whereas the weakly coupled regions are known as non-asperity and show slow and continuous slip (e.g., Lay et al. 1981; Beroza and Ide 2011).
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