Heterogeneous rheology of Japan subduction zone revealed by postseismic deformation of the 2011 Tohoku-oki earthquake
The 2011 Tohoku-oki earthquake produced the most well-recorded postseismic deformation
of any megathrust earthquake in the world. Over the last decade, researchers have used a …
of any megathrust earthquake in the world. Over the last decade, researchers have used a …
Structural control and system-level behavior of the seismic cycle at the Nankai Trough
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 …
long-term and short-term slow-slip events, slow and fast earthquakes, all associated with …
Coupled afterslip and transient mantle flow after the 2011 Tohoku earthquake
Modeling of postseismic deformation following great earthquakes has revealed the viscous
structure of the mantle and the frictional properties of the fault interface. However, for giant …
structure of the mantle and the frictional properties of the fault interface. However, for giant …
Antarctic upper mantle rheology
The Antarctic mantle and lithosphere are known to have large lateral contrasts in seismic
velocity and tectonic history. These contrasts suggest differences in the response timescale …
velocity and tectonic history. These contrasts suggest differences in the response timescale …
Dislocation creep of olivine: Backstress evolution controls transient creep at high temperatures
Transient creep occurs during geodynamic processes that impose stress changes on rocks
at high temperatures. The transient is manifested as evolution in the viscosity of the rocks …
at high temperatures. The transient is manifested as evolution in the viscosity of the rocks …
Along-arc heterogeneous rheology inferred from post-seismic deformation of the 2011 Tohoku-oki earthquake
The Japan forearc plays a crucial role in modulating the post-seismic deformation in
response to the enormous stress perturbation induced by the 2011 Tohoku-oki earthquake …
response to the enormous stress perturbation induced by the 2011 Tohoku-oki earthquake …
The seismic structure of the Antarctic upper mantle
The deployment of seismic stations and the development of ambient noise tomography as
well as new analysis methods provide an opportunity for higher-resolution imaging of …
well as new analysis methods provide an opportunity for higher-resolution imaging of …
Strong seismic anisotropy in the deep upper mantle beneath the Cascadia backarc: Constraints from probabilistic finite-frequency SKS splitting intensity tomography
P Mondal, MD Long - Earth and Planetary Science Letters, 2020 - Elsevier
Abstract The volcanically active High Lava Plains (HLP) region is a striking tectonomagmatic
feature of eastern Oregon, in the backarc of the Cascadia subduction zone. It features young …
feature of eastern Oregon, in the backarc of the Cascadia subduction zone. It features young …
Transient creep of quartz and granulite at high temperature under wet conditions
Transient creep of crustal rocks is important to explain time‐dependent geological
processes such as postseismic deformation following a large continental earthquake. While …
processes such as postseismic deformation following a large continental earthquake. While …
MCMC inversion of the transient and steady-state creep flow law parameters of dunite under dry and wet conditions
The rheology of the upper mantle impacts a variety of geodynamic processes, including
postseismic deformation following great earthquakes and post-glacial rebound. The …
postseismic deformation following great earthquakes and post-glacial rebound. The …