Sea-level rise from land subsidence in major coastal cities
Coastal land can be lost at rapid rates due to relative sea-level rise (RSLR) resulting from
local land subsidence. However, the comparative severity of local land subsidence is …
local land subsidence. However, the comparative severity of local land subsidence is …
A linear viscoelasticity for decadal to centennial time scale mantle deformation
The extended Burgers material (EBM) model provides a linear viscoelastic theory for
interpreting a variety of rock deformation phenomena in geophysics, playing an increasingly …
interpreting a variety of rock deformation phenomena in geophysics, playing an increasingly …
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 …
Three-dimensional kinematics of the India–Eurasia collision
L Wang, S Barbot - Communications Earth & Environment, 2023 - nature.com
The collision between India and Eurasia mobilizes multiple processes of continental
tectonics. However, how deformation develops within the lithosphere across the Tibetan …
tectonics. However, how deformation develops within the lithosphere across the Tibetan …
Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake
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 …
originate from the interaction of viscoelastic flow in the asthenospheric mantle and slip on …
Influence of the asthenosphere on earth dynamics and evolution
L Cathles, W Fjeldskar, A Lenardic, B Romanowicz… - Scientific Reports, 2023 - nature.com
The existence of a thin, weak asthenospheric layer beneath Earth's lithospheric plates is
consistent with existing geological and geophysical constraints, including Pleistocene glacio …
consistent with existing geological and geophysical constraints, including Pleistocene glacio …
Bayesian Inversion for a Stress‐Driven Model of Afterslip and Viscoelastic Relaxation: Method and Application to Postseismic Deformation Following the 2011 MW …
J Fukuda, KM Johnson - Journal of Geophysical Research …, 2021 - Wiley Online Library
Postseismic deformation following great subduction earthquakes is commonly modeled as
the sum of the contributions from afterslip on the megathrust and viscoelastic relaxation of …
the sum of the contributions from afterslip on the megathrust and viscoelastic relaxation of …
Illuminating subduction zone rheological properties in the wake of a giant earthquake
Deformation associated with plate convergence at subduction zones is accommodated by a
complex system involving fault slip and viscoelastic flow. These processes have proven …
complex system involving fault slip and viscoelastic flow. These processes have proven …
On computing viscoelastic Love numbers for general planetary models: the ALMA3 code
D Melini, C Saliby, G Spada - Geophysical Journal International, 2022 - academic.oup.com
The computation of the Love numbers (LNs) for a spherically symmetric self-gravitating
viscoelastic Earth is a classical problem in global geodynamics. Here we revisit the problem …
viscoelastic Earth is a classical problem in global geodynamics. Here we revisit the problem …
Finding simplicity in the complexity of postseismic coastal uplift and subsidence following great subduction earthquakes
Following great subduction earthquakes, postseismic deformation of coastal areas shows
consistent seaward motion but complex vertical deformation. Understanding both the …
consistent seaward motion but complex vertical deformation. Understanding both the …