From geodetic imaging of seismic and aseismic fault slip to dynamic modeling of the seismic cycle
JP Avouac - Annual Review of Earth and Planetary Sciences, 2015 - annualreviews.org
Understanding the partitioning of seismic and aseismic fault slip is central to seismotectonics
as it ultimately determines the seismic potential of faults. Thanks to advances in tectonic …
as it ultimately determines the seismic potential of faults. Thanks to advances in tectonic …
A review of the rupture characteristics of the 2011 Tohoku-oki Mw 9.1 earthquake
T Lay - Tectonophysics, 2018 - Elsevier
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 …
boundary megathrust fault offshore of northern Honshu with estimates of shallow slip of 50 m …
Aseismic slip and seismogenic coupling along the central San Andreas Fault
We use high‐resolution Synthetic Aperture Radar‐and GPS‐derived observations of surface
displacements to derive the first probabilistic estimates of fault coupling along the creeping …
displacements to derive the first probabilistic estimates of fault coupling along the creeping …
Resolving depth-dependent subduction zone viscosity and afterslip from postseismic displacements following the 2011 Tohoku-oki, Japan earthquake
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 …
earthquake capable of predicting postseismic displacements due to viscoelastic relaxation …
A decade of lessons learned from the 2011 Tohoku‐Oki earthquake
N Uchida, R Bürgmann - Reviews of Geophysics, 2021 - Wiley Online Library
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 …
ruptures. In the aftermath of this devastating event, it is important to learn from the complete …
Slow and fast ruptures on a laboratory fault controlled by loading characteristics
GC Mclaskey, F Yamashita - Journal of Geophysical Research …, 2017 - Wiley Online Library
Recent geodetic observations indicate that a single fault may slip slowly and silently or fast
and seismically in different circumstances. We report laboratory experiments that …
and seismically in different circumstances. We report laboratory experiments that …
[HTML][HTML] Learning from crustal deformation associated with the M9 2011 Tohoku-oki earthquake
Numerous observations pertaining to the magnitude 9.0 2011 Tohoku-oki earthquake
(offshore Japan) have led to new understanding of subduction zone earthquakes. By …
(offshore Japan) have led to new understanding of subduction zone earthquakes. By …
A model of aftershock migration driven by afterslip
Aftershocks region have been extensively reported to expand logarithmically with time. The
associated migration velocity is typically of the order of several km/decade but can be much …
associated migration velocity is typically of the order of several km/decade but can be much …
A detailed source model for the Mw9.0 Tohoku‐Oki earthquake reconciling geodesy, seismology, and tsunami records
Abstract The 11 March 2011 Mw9. 0 Tohoku‐Oki earthquake was recorded by an
exceptionally large amount of diverse data offering a unique opportunity to investigate the …
exceptionally large amount of diverse data offering a unique opportunity to investigate the …
Earthquake supercycles on the Mentawai segment of the Sunda megathrust in the seventeenth century and earlier
Over at least the past millennium, the Mentawai segment of the Sunda megathrust has failed
in sequences of closely timed events rather than in single end‐to‐end ruptures—each the …
in sequences of closely timed events rather than in single end‐to‐end ruptures—each the …