Results 141 to 150 of about 2,101 (162)
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Postseismic crustal uplift near Anchorage, Alaska

Journal of Geophysical Research, 1977
Results 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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InSAR Postseismic Displacements of the 2023 Turkey Earthquakes

The two major earthquakes (magnitude 7.8 and 7.6) in southeastern Turkey in 2023 resulted in a combined fault rupture length of 500 km. The events were driven by the northward motion of the Arabian Plate colliding with the Eurasian Plate and the westward escape of the Anatolian Plate.
Jihong Liu, Sigurjón Jónsson
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Laboratory Measurement of Permeability in Postseismic Flow

International Journal of Geomechanics, 2023
Aya Bayoumi   +2 more
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Analysis of postseismic processes

2011
Der 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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Gravitational viscoelastic postseismic relaxation on a layered spherical Earth

Journal of Geophysical Research: Solid Earth, 1997
Viscoelastic relaxation of a ductile asthenosphere underlying a purely elastic plate is a strong candidate process for explaining anomalous rates of crustal deformation observed following large earthquakes. The nongravitational treatment of Pollitz [1992], which is valid on a global scale and includes the effects of compressibility, is here extended to
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EARTHQUAKE TRIGGERING BY STATIC, DYNAMIC, AND POSTSEISMIC STRESS TRANSFER

Annual Review of Earth and Planetary Sciences, 2005
▪ Abstract  Earthquake triggering is the process by which stress changes associated with an earthquake can induce or retard seismic activity in the surrounding region or trigger other earthquakes at great distances. Calculations of static Coulomb stress changes associated with earthquake slip have proven to be a powerful tool in explaining many seismic
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Postseismic deformation following the 1991 Racha, Georgia earthquake

2010
The April 29, 1991 Racha, Georgia Mw=6.9 earthquake was the largest earthquake recorded in the western section of the Greater Caucasus Mountains. Lithospheric deformation following this earthquake was recorded by a network of eight GPS stations. These data were modeled for postseismic deformation with the mechanisms of afterslip and viscoelastic ...
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