Results 181 to 190 of about 1,989 (209)
Evidence for postseismic deformation of the lower crust following the 2004 Mw6.0 Parkfield earthquake [PDF]
Journal of Geophysical Research, 2011 Previous studies have shown that postseismic relaxation following the 2004 Mw6.0 Parkfield, CA, earthquake is dominated by afterslip. However, we show that some fraction of the afterslip inferred from kinematic inversion to have occurred immediately ...
Lucile Bruhat +2 more
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Partitioned postseismic deformation associated with the 2009 Mw 6.3 L'Aquila earthquake surface rupture measured using a terrestrial laser scanner [PDF]
Geophysical Research Letters, 2010 Using 3D terrestrial laser scan (TLS) technology, we have recorded postseismic deformation on and adjacent to the surface rupture formed during the 6th April 2009 L'Aquila normal faulting earthquake (Mw 6.3).
Ken J W Mccaffrey +2 more
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Postseismic stress diffusion in Chile and South Peru
Earth and Planetary Science Letters, 2003Abstract By means of a spherical model of global postseismic deformation we perform an analysis of the postseismic stress diffusion process associated with the main seismic events which occurred in Chile and South Peru in the last century. Our aim is to ascertain if the viscoelastic relaxation of the mantle and asthenosphere following the earthquakes,
Emanuele Casarotti
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Postseismic Mantle Relaxation in the Central Nevada Seismic Belt
Science, 2005Holocene acceleration of deformation and postseismic relaxation are two hypotheses to explain the present-day deformation in the Central Nevada Seismic Belt (CNSB). Discriminating between these two mechanisms is critical for understanding the dynamics and seismic potential of the Basin and Range province.
Noel, Gourmelen, Falk, Amelung
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Postseismic deformation after 2008 Wenchuan Earthquake
Survey Review, 2014AbstractApparent 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
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A plate flexure approximation to postseismic and interseismic deformation
Journal of Geophysical Research: Solid Earth, 1985The 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
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Interpretation of postseismic deformation with a viscoelastic relaxation model
Journal of Geophysical Research: Solid Earth, 1980Aleutian 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
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Postseismic crustal uplift near Anchorage, Alaska
Journal of Geophysical Research, 1977Results of four leveling surveys carried out by the National Geodetic Survey between Anchorage and Whittier, Alaska, combined with an analysis of sea level measurements at Anchorage, indicate as much as 0.55 m of land uplift in the decade following the 1964 Prince William Sound earthquake. The pattern of uplift is parabolic in shape, convex upward, and
Larry D. Brown +3 more
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Analysis of postseismic processes
2011Der Erdbebenzyklus ist in der Regel in drei Phasen unterteilt: die interseismische, die koseismische und die postseismische Phase. Der Großteil der interseismisch akkumulierten Spannung wird durch das Hauptbeben und die postseismischen Prozesse abgebaut.
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Laboratory Measurement of Permeability in Postseismic Flow
International Journal of Geomechanics, 2023Aya Bayoumi +2 more
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