Results 121 to 130 of about 2,101 (162)

Hillslope memory of sequential earthquakes. [PDF]

Sci Adv
Wang X, Jansen JD, Chen L, Dai L, Bhuyan K, Fang C, Nava L, Catani F, Fan X.   +8 more
europepmc   +1 more source

High-resolution co-seismic fault offsets of the 2023 Türkiye earthquake ruptures using satellite imagery. [PDF]

Sci Rep
Provost F, Karabacak V, Malet JP, Van der Woerd J, Meghraoui M, Masson F, Ferry M, Michéa D, Pointal E.   +8 more
europepmc   +1 more source

Postseismic land movements in south-central Chile

, 1990
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Postseismic relaxation and aftershocks

Journal of Geophysical Research, 2007
Perfettini et al. (2005) suggested that the temporal dependence of surface displacements u(t) measured in the epicentral area following an earthquake is related to N(t), the cumulative number of aftershocks, by the equation u(t) = a + bt + cN(t) + d(1 − e−αt), where a, b, c, d, and α are constants chosen to fit the data and t is the postearthquake time.
J. C. Savage, J. L. Svarc, Shui‐Beih Yu   +2 more
exaly   +2 more sources

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
core   +4 more sources

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, Q. B. Fan, Q. Wang, S. M. Yang, G. Y. Jiang   +4 more
exaly   +2 more sources

Omori‐like decay of postseismic velocities following continental earthquakes [PDF]

Geophysical Research Letters, 2017
Various mechanisms have been proposed to explain the transient, enhanced surface deformation rates following earthquakes. Unfortunately, these different mechanisms can produce very similar surface deformation patterns leading to difficulty in ...
Tim Wright, Tom Ingleby
exaly   +2 more sources

Capturing 50 Years of Postseismic Mantle Flow at Nankai Subduction Zone [PDF]

Journal of Geophysical Research: Solid Earth, 2018
We combine Global Positioning System, leveling, and tide gauge records of vertical motion in southwest Japan spanning postseismic deformation following the 1944 M8.1 Tonankai and 1946 M8.4 Nankai earthquakes.
Kaj Johnson
exaly   +3 more sources

Postseismic Viscoelastic Rebound

Science, 1974
The sudden appearance of a dislocation, representing an earthquake, in an elastic layer (the lithosphere) overriding a viscoelastic half space (the asthenosphere) is followed by time-dependent surface deformation, which is very similar to in situ postseismic deformation.
A, Nur, G, Mavko
openaire   +2 more sources