Both dip and thickness influence the recovery.
The shape of this distribution makes sense because the response is sensitive to the length, dip, and thickness; all of which have a normal distribution.
Furthermore, based on the numerical analysis results, the location, dip and thickness of the interlayer as well as the distance from the interlayer to the tunnel were proved to be important factors influencing tunnel stability, and the relationships of the induced damage zones with these parameters of the weak interlayer were established.
When the main failure surface is contained within a weak horizon, the dip and thickness of the weak horizon have a positive effect on the displacement of the failure mass, whereas a shallow-located weak horizon causes larger displacement of the failure mass during the collapse of granular slopes.
However other factors can influence the temperature field and, thus, the slab dehydration processes, such as the slab dip, the thickness of the overriding plate, the rheology of the mantle wedge, and the composition of subducting plate.
The (epsilon _mathrm{{r}}) is more sensitive to the dip angle than thickness (Fig. 6b).
The heat recovery from the regular design improves as the reservoir length, dip angle, or thickness increase.
The distribution of these internal structures within the failure mass is affected significantly by the dip, location and thickness of the weak horizon.
In this study, we use results of analogue models to investigate the effect of the dip, location and thickness of a weak horizon on the stability/failure, kinematics and internal deformation of a granular slope.
The convergence of the Levenberg-Marquardt method and its corresponding inverse parameters (e.g., the depth, dip angle, and thickness of the buried target) obtained from each window were plotted in their paper.
