This paper summarizes the results of 10 years of research on models of the megathrust
earthquake cycles and crustal deformation associated with the 2011 Tohoku-oki earthquake …

The deformation transient following large subduction zone earthquakes is thought to
originate from the interaction of viscoelastic flow in the asthenospheric mantle and slip on …

The diverse mechanical behaviors of subduction zones during the seismic cycle emerge
from the nonlinear dynamics of a complex mechanical system with interacting brittle and …

Abstract The Nankai Trough in Southwest Japan exhibits a wide spectrum of fault slip, with
long-term and short-term slow-slip events, slow and fast earthquakes, all associated with …

Subduction megathrusts develop the largest earthquakes, often close to large population
centers. Understanding the dynamics of deformation at subduction zones is therefore …

The surface deformation associated with the 2010 M w 8.8 Maule earthquake in Chile was
recorded in great detail before, during and after the event. The high data quality of the …

We have developed an inversion method for estimating 3-D tectonic stress fields from
centroid moment tensor (CMT) data of seismic events. To obtain reliable inversion analysis …

The fully relaxed deformation caused by an earthquake refers to the total deformation of the
earth caused by the earthquake, including the coseismic deformation and the total effect of …

We use 2018–2020 Sentinel-1 InSAR time series data to study post-seismic deformation
processes following the 2017 Mw 7.3 Kermanshah, Iraq earthquake. We remove …

We detected the mechanically coupled areas, or high stress rate patches, on the plate
interface in the Kanto region, central Japan, by analyzing the Global Navigation Satellite …