Abstract The 2011 March 11 Tohoku-oki great (Mw 9.1) earthquake ruptured the plate
boundary megathrust fault offshore of northern Honshu with estimates of shallow slip of 50 m …

Abstract The 2011 Mw 9.0 Tohoku‐oki earthquake is one of the world's best‐recorded
ruptures. In the aftermath of this devastating event, it is important to learn from the complete …

We estimate the rates and patterns of vertical land motion (VLM) on all locations on Earth's
land surface using GPS Imaging. The solution is based on a large database of uniformly …

We analyze three‐dimensional GPS coordinate time series from continuously operating
stations in Nepal and South Tibet and calculate the initial 1 year postseismic displacements …

We developed a 3-D, viscoelastic finite element model of the M9 2011 Tohoku-oki, Japan
earthquake capable of predicting postseismic displacements due to viscoelastic relaxation …

Understanding of postseismic deformation following great subduction zone earthquakes is
complicated by the combined effects of viscoelastic relaxation of earthquake‐induced …

The Himalayan arc produced the largest known continental earthquake, the Mw≈ 8.7
Assam earthquake of 1950, but how frequently and where else in the Himalaya such large …

Megathrust earthquakes of magnitude close to 9 are followed by large-scale (thousands of
km) and long-lasting (decades), significant crustal and mantle deformation. This deformation …

Large interplate earthquakes are often followed by postseismic slip that is considered to
occur in areas surrounding the coseismic ruptures. Such spatial separation is expected from …

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 …