Thus, to fit the data requires slip increase in LYR and slip decrease in SLAB.
The slip direction is parallel to line ab in Fig. 4, and slip decreases linearly from 40 m at the center to zero at the distance of 200 km.
It was found that the shear failure loads of bonding slip decreased successively with more loading cycles of the repeated push-out test employed in the same direction.
The reductions of the shear capacity and the shear slip decreased approximately with the increase of tie-bar diameter, and they were 28 42% and 58 67%, respectively.
The fault gradually terminates as slip decreases with depth.
To the contrary, the result shows the maximum slip decreases for the combined inversion case.
Taper the slip distribution by adding three rows and columns over which slip decreases to zero on each side of the fault plane.
The critical resolved shear stress (CRSS) for (001)<110> slip decreases with increasing temperature, exhibiting a moderate peak (or plateau) in the temperature range from 800 to 1100 °C.
Furthermore, studies on dislocation fault models have indicated that stress discontinuity across a fault can occur where slip decreases or increases along the fault plane (e.g., Maruyama 1969).
Compared to the results for the combined inversion, the slip in HOM is more broadly distributed, and the maximum slip decreases to 22.4 m, which is consistent with other studies without offshore data (Ozawa et al. 2011; Iinuma et al. 2011).
