Fig. 2From: The nature of the Pacific plate as subduction inputs to the northeastern Japan arc and its implication for subduction zone processesTime-migrated seismic reflection profiles in the outer trench area of lines A2, A3, and A4 showing horst and graben structure developed by faulting related to plate bending (Fujie et al. 2013b, 2018, 2020)Back to article page