Author Posting. © The Authors, 2014. This article is posted here by permission of The Royal Astronomical Society for personal use, not for redistribution. The definitive version was published in Geophysical Journal International 197 (2014): 697-704, doi:10.1093/gji/ggu048.After the 1960 M9.5 Valdivia, Chile earthquake, three types of geodetic observations were made during four time periods at nearby locations. These post-seismic observations were previously explained by post-seismic afterslip on the downdip extension of the 1960 rupture plane. In this study, we demonstrate that the post-seismic observations can be explained alternatively by volumetric viscoelastic relaxation of the asthenosphere mantle. In searching for the best-fitting v...
International audienceThe postseismic deformation following a large (Mw >7) earthquake is expressed ...
International audienceThe postseismic deformation following a large (Mw >7) earthquake is expressed ...
The postseismic deformation following a large (M-w>7) earthquake is expressed both seismically and a...
We develop a three-dimensional viscoelastic finite element model to study postseismic deformation as...
The 2005 Mw 7.8 Tarapaca earthquake was the result of normal faulting on a west-dipping plane at a d...
Spatial and temporal measurements from satellite geodesy observations provide fundamental constraint...
Contemporary crustal deformation of the southern Andean margin shows an interesting feature: While n...
The 2005 M-w 7.8 Tarapaca earthquake was the result of normal faulting on a west-dipping plane at a ...
The 2005 M-w 7.8 Tarapaca earthquake was the result of normal faulting on a west-dipping plane at a ...
Deformation associated with plate convergence at subduction zones is accommodated by a complex syste...
International audienceSUMMARY Over the last decade, three major subduction earthquakes, Maule Mw 8.8...
Large intraplate subduction earthquakes are generally accompanied by prolonged and intense postseism...
International audienceMegathrust earthquakes of magnitude close to 9 are followed by large-scale (th...
[1] We develop a three-dimensional viscoelastic finite element model to study postseismic deformatio...
The postseismic deformation captured with continuous Global Positioning System (cGPS) monitoring fol...
International audienceThe postseismic deformation following a large (Mw >7) earthquake is expressed ...
International audienceThe postseismic deformation following a large (Mw >7) earthquake is expressed ...
The postseismic deformation following a large (M-w>7) earthquake is expressed both seismically and a...
We develop a three-dimensional viscoelastic finite element model to study postseismic deformation as...
The 2005 Mw 7.8 Tarapaca earthquake was the result of normal faulting on a west-dipping plane at a d...
Spatial and temporal measurements from satellite geodesy observations provide fundamental constraint...
Contemporary crustal deformation of the southern Andean margin shows an interesting feature: While n...
The 2005 M-w 7.8 Tarapaca earthquake was the result of normal faulting on a west-dipping plane at a ...
The 2005 M-w 7.8 Tarapaca earthquake was the result of normal faulting on a west-dipping plane at a ...
Deformation associated with plate convergence at subduction zones is accommodated by a complex syste...
International audienceSUMMARY Over the last decade, three major subduction earthquakes, Maule Mw 8.8...
Large intraplate subduction earthquakes are generally accompanied by prolonged and intense postseism...
International audienceMegathrust earthquakes of magnitude close to 9 are followed by large-scale (th...
[1] We develop a three-dimensional viscoelastic finite element model to study postseismic deformatio...
The postseismic deformation captured with continuous Global Positioning System (cGPS) monitoring fol...
International audienceThe postseismic deformation following a large (Mw >7) earthquake is expressed ...
International audienceThe postseismic deformation following a large (Mw >7) earthquake is expressed ...
The postseismic deformation following a large (M-w>7) earthquake is expressed both seismically and a...