Abstract:Based on dislocation theory of Okada, we adopted a finite-element fault model inverted by Gavin Hayes from seismic data for the 2011 Japan Mw9.0 earthquake, and obtained the corresponding surface displacement and strain fields. The calculated displacement field is consistent with the observed GPS results in the trend of changes. Also the surface displacement and strain fields both show large variations in space
The coseismic slip distribution of the Mw 9.0 2011 Tohoku-Oki earthquake has been estimated by inver...
We calculated surface displacements produced by a synthetic megathrust earthquake using two spherica...
The 11 March 2011 Tohoku earthquake was the strongest event recorded in recent historic seismicity i...
Based on dislocation theory of Okada, we adopted a finite-element fault model inverted by Gavin Haye...
Abstract:Based on dislocation theory of Okada, we adopted a finite-element fault model inverted by G...
Abstract:Co-seismic displacements associated with the Mw9. 0 earthquake on March 11, 2011 in Japan a...
Co-seismic displacements associated with the Mw9. 0 earthquake on March 11, 2011 in Japan are numeri...
The three-dimensional crustal displacement field as sampled by GPS is used to determine the coseismi...
The distribution of slip faults along the fault plane plays a special role in the kinetic pattern of...
Abstract:Theoretical horizontal displacements caused by the 2004 Sumatra earthquake in the Sichuan-Y...
Theoretical horizontal displacements caused by the 2004 Sumatra earthquake in the Sichuan-Yunnan are...
Abstract:Co-seismic displacements associated with the Mw9. 0 earthquake on March 11, 2011 in Japan a...
Numerical simulations based on continuum mechanics are promising methods for the estimation of surfa...
The residual displacement and strain fields are computed at the free surface of a non-gravitating, h...
For this study, we conducted a numerical simulation on co-seismic displacement for a dip-slip fault ...
The coseismic slip distribution of the Mw 9.0 2011 Tohoku-Oki earthquake has been estimated by inver...
We calculated surface displacements produced by a synthetic megathrust earthquake using two spherica...
The 11 March 2011 Tohoku earthquake was the strongest event recorded in recent historic seismicity i...
Based on dislocation theory of Okada, we adopted a finite-element fault model inverted by Gavin Haye...
Abstract:Based on dislocation theory of Okada, we adopted a finite-element fault model inverted by G...
Abstract:Co-seismic displacements associated with the Mw9. 0 earthquake on March 11, 2011 in Japan a...
Co-seismic displacements associated with the Mw9. 0 earthquake on March 11, 2011 in Japan are numeri...
The three-dimensional crustal displacement field as sampled by GPS is used to determine the coseismi...
The distribution of slip faults along the fault plane plays a special role in the kinetic pattern of...
Abstract:Theoretical horizontal displacements caused by the 2004 Sumatra earthquake in the Sichuan-Y...
Theoretical horizontal displacements caused by the 2004 Sumatra earthquake in the Sichuan-Yunnan are...
Abstract:Co-seismic displacements associated with the Mw9. 0 earthquake on March 11, 2011 in Japan a...
Numerical simulations based on continuum mechanics are promising methods for the estimation of surfa...
The residual displacement and strain fields are computed at the free surface of a non-gravitating, h...
For this study, we conducted a numerical simulation on co-seismic displacement for a dip-slip fault ...
The coseismic slip distribution of the Mw 9.0 2011 Tohoku-Oki earthquake has been estimated by inver...
We calculated surface displacements produced by a synthetic megathrust earthquake using two spherica...
The 11 March 2011 Tohoku earthquake was the strongest event recorded in recent historic seismicity i...