Fig. 6: A schematic view of the fault system and deep structure beneath the Noto Peninsula and Toyama Trough.
From: Sub-parallel fault afterslip and weak zone relaxation after the 2024 Noto earthquake
A Fault slip behaviors of the coseismic fault and the possible hidden fault, and the viscoelastic weak zone beneath the Toyama Trough. Aseismic slip area is modified from Yoshida et al.45. B A cross-section view across the fault system and deep structure.
