Abstract:Co-seismic displacements associated with the Mw9. 0 earthquake on March 11, 2011 in Japan are numerically simulated on the basis of a finite-fault dislocation model with PSGRN/PSCMP software. Compared with the inland GPS observation, 90% of the computed eastward, northward and vertical displacements have residuals less than 0.10 m, suggesting that the simulated results can be, to certain extent, used to demonstrate the co-seismic deformation in the near field. In this model, the maximum eastward displacement increases from 6 m along the coast to 30 m near the epicenter, where the maximum southward displacement is 13 m. The three-dimensional display shows that the vertical displacement reaches a maximum uplift of 14.3 m, which is co...
Abstract:Based on dislocation theory of Okada, we adopted a finite-element fault model inverted by G...
Abstract:Surface co-seismic gravity changes and displacements caused by the Wenchuan Ms8. 0 earthqua...
Great earthquakes introduce measurable co-seismic displacements over regions of hundreds and thousan...
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...
Abstract:Based on dislocation theory of Okada, we adopted a finite-element fault model inverted by G...
The distribution of slip faults along the fault plane plays a special role in the kinetic pattern of...
The three-dimensional crustal displacement field as sampled by GPS is used to determine the coseismi...
The 11 March 2011 Tohoku earthquake was the strongest event recorded in recent historic seismicity i...
Abstract:Theoretical horizontal displacements caused by the 2004 Sumatra earthquake in the Sichuan-Y...
The 11 March 2011 Tohoku earthquake was the strongest event recorded in recent historic seismicity i...
Abstract:Using plane dislocation theory and the seismic-wave inversion results from the Institute of...
The 17 January 1994 Northridge, California, earthquake significantly deformed the Earth's crust in t...
The 17 January 1994 Northridge, California, earthquake significantly deformed the Earth's crust in t...
This paper presents and discusses the global co-seismic displacements caused by the 2004 Sumatra-And...
Abstract:Based on dislocation theory of Okada, we adopted a finite-element fault model inverted by G...
Abstract:Surface co-seismic gravity changes and displacements caused by the Wenchuan Ms8. 0 earthqua...
Great earthquakes introduce measurable co-seismic displacements over regions of hundreds and thousan...
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...
Abstract:Based on dislocation theory of Okada, we adopted a finite-element fault model inverted by G...
The distribution of slip faults along the fault plane plays a special role in the kinetic pattern of...
The three-dimensional crustal displacement field as sampled by GPS is used to determine the coseismi...
The 11 March 2011 Tohoku earthquake was the strongest event recorded in recent historic seismicity i...
Abstract:Theoretical horizontal displacements caused by the 2004 Sumatra earthquake in the Sichuan-Y...
The 11 March 2011 Tohoku earthquake was the strongest event recorded in recent historic seismicity i...
Abstract:Using plane dislocation theory and the seismic-wave inversion results from the Institute of...
The 17 January 1994 Northridge, California, earthquake significantly deformed the Earth's crust in t...
The 17 January 1994 Northridge, California, earthquake significantly deformed the Earth's crust in t...
This paper presents and discusses the global co-seismic displacements caused by the 2004 Sumatra-And...
Abstract:Based on dislocation theory of Okada, we adopted a finite-element fault model inverted by G...
Abstract:Surface co-seismic gravity changes and displacements caused by the Wenchuan Ms8. 0 earthqua...
Great earthquakes introduce measurable co-seismic displacements over regions of hundreds and thousan...