Fig. 2: Contribution of viscoelastic deformation in response to different motions on the fault.
From: Sub-parallel fault afterslip and weak zone relaxation after the 2024 Noto earthquake
A, B viscoelastic deformation contributed from strike-slip and dip-slip components of the coseismic slip, respectively. C The sum of (A, B). D, E, F, respectively, represent observations, models, and model residuals. Arrows represent the horizontal displacements. The contour lines are the vertical displacements. The effects of a weak zone and of afterslip in controlling surface deformation have not been considered yet.
