Results 91 to 100 of about 264 (129)
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The role of rheological heterogeneities in postseismic deformation

2022
<p>Advances in modelling and access to InSAR and GNSS observations have highlighted the role that rheological heterogeneities play in postseismic deformation. Here we discuss three recent studies (Muto et al. 2019, Sambuddha et al. 2022, and Takada et al.
James Moore   +4 more
openaire   +1 more source

Postseismic deformation after 2008 Wenchuan Earthquake

Survey Review, 2014
AbstractApparent postseismic deformation was observed after the 2008 Wenchuan earthquake, China. The displacement in the direction normal to the fault decays to nearly zero after 2013, but the significant dextral movement did not decay obviously during our observation of up to May 2013.
C. J. Xu   +4 more
exaly   +2 more sources

Postseismic Deformation Monitoring With the COSMO/SKYMED Constellation

IEEE Geoscience and Remote Sensing Letters, 2011
COSMO/SKYMED is currently the unique constellation of synthetic aperture radar (SAR) sensors operative, which is also for civilian use. On April 6, 2009, an Mw 6.3 earthquake struck the city of I'Aquila in Central Italy. The constellation acquired data stacks over the hit area at an unprecedented temporal rate.
Diego Reale   +5 more
openaire   +5 more sources

Vertical Postseismic Deformation of the 2019 Ridgecrest Earthquake Sequence

Journal of Geophysical Research: Solid Earth, 2022
AbstractThe 2019 Ridgecrest conjugate Mw6.4 and Mw7.1 events resulted in several meters of strike‐slip and dip‐slip along an intricate rupture, extending from the surface down to 15 km. Now with >2 years of post‐rupture observations, we utilize these results to better understand vertical postseismic deformation from the Ridgecrest sequence and ...
Lauren A. Ward   +5 more
openaire   +1 more source

Global postseismic deformation: Deep earthquakes

Journal of Geophysical Research: Solid Earth, 2000
We study the global viscoelastic deformations associated with a shear dislocation on a fault embedded in a viscoelastic mantle. To address this problem, we extend the theory of the quasi‐static deformations of a Maxwell, spherical, N‐layer incompressible Earth, previously limited to the modeling of the effects of earthquakes occurring only within the ...
L. Boschi, A. Piersanti, SPADA, GIORGIO
openaire   +2 more sources

Interpretation of postseismic deformation with a viscoelastic relaxation model

Journal of Geophysical Research: Solid Earth, 1980
Aleutian tide gages registered coseismic subsidence of 10–15 cm at three locations during the great earthquakes of 1957 and 1965. For approximately 5–6 years after this initial subsidence the data indicate postseismic uplift of the islands to approximately their initial level.
J. Wahr, M. Wyss
openaire   +1 more source

A plate flexure approximation to postseismic and interseismic deformation

Journal of Geophysical Research: Solid Earth, 1985
The rather large postseismic deformation that is associated with two‐dimensional dip‐slip faulting in the lithosphere is related to the bending of a free plate generated by dip‐slip faulting. In the absence of gravity, asthenosphere relaxation eventually permits the faulted lithosphere to assume the dihedral configuration of a faulted free plate.
J. C. Savage, Guohua Gu
openaire   +1 more source

Izmit earthquake postseismic deformation and dynamics of the North Anatolian Fault Zone [PDF]

open access: yesJournal of Geophysical Research, 2009
We have modeled postseismic deformation from 1999 to 2003 in the region surrounding the 1999 Izmit and Düzce earthquake ruptures, using a three‐dimensional viscoelastic finite element method. Our models confirm earlier findings that surface deformation within the first few months of the Izmit earthquake is principally due to stable frictional afterslip
Semih Ergintav, Simon McClusky
exaly   +4 more sources

A viscoelastic and afterslip postseismic deformation model for the 1964 Alaska earthquake [PDF]

open access: yesJournal of Geophysical Research, 2009
We developed a 3‐D viscoelastic model, in concert with an afterslip model, to describe the postseismic deformation following the 1964 Alaska earthquake. Our model incorporates a realistic geometry including an elastic slab with very low dip angle. These geometric factors are important and require a reanalysis of the 1964 coseismic model.
Jeffrey Freymueller, Hisashi Suito
exaly   +2 more sources

Spherical versus flat models of coseismic and postseismic deformations

Journal of Geophysical Research: Solid Earth, 1999
We perform an exhaustive study of coseismic and postseismic surface deformations induced by shear dislocations using flat and spherical Earth models. Our aim is to examine the effects of the spherical geometry, the vertical layering, and the self‐gravitation on surface displacement field.
C. Nostro   +3 more
openaire   +1 more source

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