Results 31 to 40 of about 22,222 (295)

Two‐stage composite megathrust rupture of the 2015 Mw8.4 Illapel, Chile, earthquake identified by spectral‐element inversion of teleseismic waves

open access: yesGeophysical Research Letters, 2016
The Mw8.4 Illapel earthquake occurred on 16 September was the largest global event in 2015. This earthquake was not unexpected because the hypocenter was located in a seismic gap of the Peru‐Chile subduction zone. However, the source model derived from 3‐
Shiann‐Jong Lee   +5 more
doaj   +1 more source

Analogue earthquakes and seismic cycles: experimental modelling across timescales [PDF]

open access: yesSolid Earth, 2017
Earth deformation is a multi-scale process ranging from seconds (seismic deformation) to millions of years (tectonic deformation). Bridging short- and long-term deformation and developing seismotectonic models has been a challenge in experimental ...
M. Rosenau   +3 more
doaj   +1 more source

Statistical physics of earthquakes: Comparison of distribution exponents for source area and potential energy and the dynamic emergence of log-periodic energy quanta [PDF]

open access: yes, 2000
We investigate the relationship between the size distribution of earthquake rupture area and the underlying elastic potential energy distribution in a cellular automaton model for earthquake dynamics.
Amelung   +52 more
core   +1 more source

Role of fault branches in earthquake rupture dynamics [PDF]

open access: yesJournal of Geophysical Research: Solid Earth, 2007
We analyze earthquake ruptures propagating along a straight “main” fault and encountering a finite‐length branch fault. Such intersections are often observed in natural fault systems. The predicted effects of the interaction with the branch that we report can be remarkable; they can strongly perturb the propagation velocity on the main fault and, in ...
Bhat, Harsha S.   +3 more
openaire   +2 more sources

On the contribution of the horizontal sea-bed displacements into the tsunami generation process [PDF]

open access: yes, 2012
The main reason for the generation of tsunamis is the deformation of the bottom of the ocean caused by an underwater earthquake. Usually, only the vertical bottom motion is taken into account while the horizontal co-seismic displacements are neglected in
Ammon   +90 more
core   +3 more sources

Deformation due to the 17 August 1999 Izmit, Turkey, earthquake measured from SPOT images [PDF]

open access: yes, 2002
The geometry of the ruptured areas and the coseismic slip distribution data are key to highlighting the behavior of seismic faults. This information is generally retrieved from field investigations and geodetic measurements or synthetic aperture radar ...
Avouac, Jean-Philippe, Michel, Rémi
core   +1 more source

Dynamic earthquake rupture preserved in a creeping serpentinite shear zone [PDF]

open access: yesNature Communications, 2018
AbstractLaboratory experiments on serpentinite suggest that extreme dynamic weakening at earthquake slip rates is accompanied by amorphisation, dehydration and possible melting. However, hypotheses arising from experiments remain untested in nature, because earthquake ruptures have not previously been recognised in serpentinite shear zones.
Matthew S. Tarling   +3 more
openaire   +5 more sources

Earthquake Stress Drops From Dynamic Rupture Simulations Constrained by Observed Ground Motions

open access: yesGeophysical Research Letters, 2020
Stress drop characterizing dynamics of earthquake rupture propagation has various definitions and measures with a yet unclear mutual relationship. We aim to reconcile this discrepancy by analyzing synthetic dynamic rupture models generated by random ...
F. Gallovič, Ľ. Valentová
doaj   +1 more source

Earthquake-induced fracture displacements and transmissivity changes in a 3D fracture network of crystalline rock for spent nuclear fuel disposal

open access: yesJournal of Rock Mechanics and Geotechnical Engineering, 2023
During the long service period of a nuclear waste repository in crystalline rock, large earthquake(s) may occur nearby the repository site and coseismically alter the local stress field around pre-existing fractures within the geological formation.
Wenbo Pan   +3 more
doaj   +1 more source

Tsunami generation by dynamic displacement of sea bed due to dip-slip faulting [PDF]

open access: yes, 2008
In classical tsunami-generation techniques, one neglects the dynamic sea bed displacement resulting from fracturing of a seismic fault. The present study takes into account these dynamic effects.
Benkhaldoun   +24 more
core   +3 more sources

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