AbstractTo improve the accuracy of inverse analysis of earthquake fault slip distribution, we performed several hundred analyses using a 108-degree-of-freedom finite element (FE) model of the crustal structure in an efficient way based on capacity computing. we developed a meshing method and an efficient computational method for these large FE models, which methods are specialized for the problem setting. We applied the model to the inverse analysis of coseismic fault slip distribution for the 2011 Tohoku-oki Earthquake. The high resolution of our model provided a significant improvement of the fidelity of the simulation results compared to existing computational approaches
In the literature, the inverted coseismic slip models from seismological and geodetic data for the 2...
Fault slip distribution is usually retrieved from geodetic data assuming that the local crust is an ...
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...
The coseismic slip distribution of the Mw 9.0 2011 Tohoku-Oki earthquake has been estimated by inve...
The 11 March 2011 Tohoku earthquake was the strongest event recorded in recent historic seismicity i...
We present a Finite Element inverse analysis of the static deformation field for the Mw= 6.3, 2009 L...
We invert InSAR from ascending and descending passes of ENVISAT/ASAR data to estimate the distributi...
Subduction is responsible for the most powerful earthquakes and dangerous volcanic eruptions, result...
ruptured the interface separating the subducting Indo-Australian plate from the overriding Burma pla...
The distribution of slip faults along the fault plane plays a special role in the kinetic pattern of...
Earthquakes cause lasting changes in static equilibrium, resulting in global deformation fields that...
Numerical simulations based on continuum mechanics are promising methods for the estimation of surfa...
The three-dimensional crustal displacement field as sampled by GPS is used to determine the coseismi...
Since huge earthquakes are expected along plate subduction zones such as the Japan Trench and Nankai...
In the literature, the inverted coseismic slip models from seismological and geodetic data for the 2...
Fault slip distribution is usually retrieved from geodetic data assuming that the local crust is an ...
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...
The coseismic slip distribution of the Mw 9.0 2011 Tohoku-Oki earthquake has been estimated by inve...
The 11 March 2011 Tohoku earthquake was the strongest event recorded in recent historic seismicity i...
We present a Finite Element inverse analysis of the static deformation field for the Mw= 6.3, 2009 L...
We invert InSAR from ascending and descending passes of ENVISAT/ASAR data to estimate the distributi...
Subduction is responsible for the most powerful earthquakes and dangerous volcanic eruptions, result...
ruptured the interface separating the subducting Indo-Australian plate from the overriding Burma pla...
The distribution of slip faults along the fault plane plays a special role in the kinetic pattern of...
Earthquakes cause lasting changes in static equilibrium, resulting in global deformation fields that...
Numerical simulations based on continuum mechanics are promising methods for the estimation of surfa...
The three-dimensional crustal displacement field as sampled by GPS is used to determine the coseismi...
Since huge earthquakes are expected along plate subduction zones such as the Japan Trench and Nankai...
In the literature, the inverted coseismic slip models from seismological and geodetic data for the 2...
Fault slip distribution is usually retrieved from geodetic data assuming that the local crust is an ...
For this study, we conducted a numerical simulation on co-seismic displacement for a dip-slip fault ...