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 …
A decade of lessons learned from the 2011 Tohoku‐Oki earthquake
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 …
Viscoelastic relaxation following subduction earthquakes and its effects on afterslip determination
Afterslip is commonly thought to be the controlling process in postseismic deformation
immediately following a great megathrust earthquake and is usually inferred from geodetic …
immediately following a great megathrust earthquake and is usually inferred from geodetic …
Afterslip and viscoelastic relaxation following the 2011 Tohoku‐oki earthquake (Mw9.0) inferred from inland GPS and seafloor GPS/Acoustic data
S Yamagiwa, S Miyazaki, K Hirahara… - Geophysical …, 2015 - Wiley Online Library
We simultaneously estimate 2.5 years of afterslip and viscoelastic relaxation, as well as
coseismic slip, for the 2011 Tohoku‐oki earthquake. Displacements at inland GPS and …
coseismic slip, for the 2011 Tohoku‐oki earthquake. Displacements at inland GPS and …
Seafloor observations indicate spatial separation of coseismic and postseismic slips in the 2011 Tohoku earthquake
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 …
occur in areas surrounding the coseismic ruptures. Such spatial separation is expected from …
[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 …
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 …
Post-seismic deformation following the 2011 Mw9.0 Tohoku–Oki earthquake and its impact on Northeast Asia
T Liu, G Fu, Y She, G Meng, Z Zou, W Wu… - Geophysical Journal …, 2023 - academic.oup.com
The objective of this study was to examine co-and post-seismic deformation following the
2011 M w9. 0 Tohoku–Oki earthquake and its impact on Northeast Asia. Large-scale, long …
2011 M w9. 0 Tohoku–Oki earthquake and its impact on Northeast Asia. Large-scale, long …
Correlation between Coulomb stress imparted by the 2011 Tohoku-Oki earthquake and seismicity rate change in Kanto, Japan
We studied the seismicity rate increase in the Kanto region around Tokyo following the 2011
Tohoku-Oki earthquake (M w 9.0) to examine whether this increase was correlated with the …
Tohoku-Oki earthquake (M w 9.0) to examine whether this increase was correlated with the …
Improvement on spatial resolution of a coseismic slip distribution using postseismic geodetic data through a viscoelastic inversion
Obvious crustal deformation is observed during a postseismic period as well as a coseismic
period associated with a large earthquake. Major mechanisms of transient postseismic …
period associated with a large earthquake. Major mechanisms of transient postseismic …