Achievements and prospects of global broadband seismographic networks after 30 years of continuous geophysical observations
Global seismographic networks (GSNs) emerged during the late nineteenth and early
twentieth centuries, facilitated by seminal international developments in theory, technology …
twentieth centuries, facilitated by seminal international developments in theory, technology …
Physical applications of GPS geodesy: A review
Geodesy, the oldest science, has become an important discipline in the geosciences, in
large part by enhancing Global Positioning System (GPS) capabilities over the last 35 years …
large part by enhancing Global Positioning System (GPS) capabilities over the last 35 years …
Time and space distribution of coseismic slip of the 2011 Tohoku earthquake as inferred from tsunami waveform data
K Satake, Y Fujii, T Harada… - Bulletin of the …, 2013 - pubs.geoscienceworld.org
A multiple time window inversion of 53 high‐sampling tsunami waveforms on ocean‐bottom
pressure, Global Positioning System, coastal wave, and tide gauges shows a temporal and …
pressure, Global Positioning System, coastal wave, and tide gauges shows a temporal and …
Seafloor geodetic constraints on interplate coupling of the Nankai Trough megathrust zone
Y Yokota, T Ishikawa, S Watanabe, T Tashiro, A Asada - Nature, 2016 - nature.com
Interplate megathrust earthquakes have inflicted catastrophic damage on human society.
Such an earthquake is predicted to occur in the near future along the Nankai Trough off …
Such an earthquake is predicted to occur in the near future along the Nankai Trough off …
Prevalence of viscoelastic relaxation after the 2011 Tohoku-oki earthquake
After a large subduction earthquake, crustal deformation continues to occur, with a complex
pattern of evolution. This postseismic deformation is due primarily to viscoelastic relaxation …
pattern of evolution. This postseismic deformation is due primarily to viscoelastic relaxation …
Episodic slow slip events in the Japan subduction zone before the 2011 Tohoku-Oki earthquake
We describe two transient slow slip events that occurred before the 2011 Tohoku-Oki
earthquake. The first transient crustal deformation, which occurred over a period of a week in …
earthquake. The first transient crustal deformation, which occurred over a period of a week in …
[HTML][HTML] Subduction zone megathrust earthquakes
Subduction zone megathrust faults host Earth's largest earthquakes, along with multitudes of
smaller events that contribute to plate convergence. An understanding of the faulting …
smaller events that contribute to plate convergence. An understanding of the faulting …
Coseismic slip distribution of the 2011 off the Pacific Coast of Tohoku Earthquake (M9. 0) refined by means of seafloor geodetic data
On 11 March 2011, the devastating M9. 0 Tohoku Earthquake occurred on the interface of
the subducting Pacific plate, and was followed by a huge tsunami that killed about 20,000 …
the subducting Pacific plate, and was followed by a huge tsunami that killed about 20,000 …
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 …
Quasi real‐time fault model estimation for near‐field tsunami forecasting based on RTK‐GPS analysis: Application to the 2011 Tohoku‐Oki earthquake (Mw 9.0)
Y Ohta, T Kobayashi, H Tsushima… - Journal of …, 2012 - Wiley Online Library
Real‐time crustal deformation monitoring is extremely important for achieving rapid
understanding of actual earthquake scales, because the measured permanent displacement …
understanding of actual earthquake scales, because the measured permanent displacement …