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Study on non-tectonic gravity effects in western Shandong. [PDF]
Sci RepLi S +6 more
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Helium isotope anomaly in groundwater prior to the 2024 Noto Peninsula earthquake. [PDF]
Nat CommunKagoshima T +8 more
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Post-seismic deformations associated with 1995 Mw8.0 Antofagasta and 1960 Mw9.5 Chile earthquakes
, 2001 G. Khazaradze, Juergen Klotz
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Post-seismic viscoelastic deformation
Acta Geodaetica et Geophysica Hungarica, 2002The 3D quasi-static displacements during and following an earthquake provide a wealth of information on the internal structure and rheological properties of the Earth. If an earthquake occurs in a region that has shallow-viscosity zones inside the crust or at the top of the mantle (asthenosphere), then post-seismic displacements of the crust on the ...
Vermeersen, L. L. A. +2 more
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Post-seismic deformation associated with the 2001 Bhuj earthquake
Natural Hazards, 2012We report the results of GPS measurements of post-seismic deformation due to the 2001 Bhuj earthquake in the Kachchh region, western India. The estimated horizontal velocity vectors in ITRF05 are in the range of 48–49 mm/year in N46–50°E. The observed velocity at the Gandhinagar permanent site, a far off site from the earthquake source region and ...
Pallabee Choudhury +5 more
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2016
The occurrence of faulting in the lithosphere is responsible for an instantaneous deformation of the Earth’s surface, which is called co-seismic deformation. In response to the induced elastic stress in the mantle, creep occurs in this deep portion of the planet, or in the ductile portion of the crust, via viscoelastic stress relaxation.
Roberto Sabadini +2 more
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The occurrence of faulting in the lithosphere is responsible for an instantaneous deformation of the Earth’s surface, which is called co-seismic deformation. In response to the induced elastic stress in the mantle, creep occurs in this deep portion of the planet, or in the ductile portion of the crust, via viscoelastic stress relaxation.
Roberto Sabadini +2 more
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Kick‐and‐cook experiments on peridotite: simulating coseismic deformation and post‐seismic creep
Terra Nova, 2011Terra Nova, 24, 62–69, 2012AbstractExperiments comprising deformation at 600 °C and annealing at 700–1000 °C were performed on natural peridotite to examine the microfabric evolution at conditions corresponding to those prevailing just below the seismogenic zone in suboceanic upper mantle.
Anthony Druiventak +3 more
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pure and applied geophysics, 1977
We present a realistic model of the San Andreas fault zone. We propose that aseismic ground displacement is a sum of visco-elastic relaxation following large earthquakes, transient fault slip, steady fault slip and a large-scale relative plate motion.
John B. Rundle, David D. Jackson
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We present a realistic model of the San Andreas fault zone. We propose that aseismic ground displacement is a sum of visco-elastic relaxation following large earthquakes, transient fault slip, steady fault slip and a large-scale relative plate motion.
John B. Rundle, David D. Jackson
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Study on Post-Seismic Deformation of Two Strong Earthquakes Occurred in Northern Tibet Plateau
IGARSS 2019 - 2019 IEEE International Geoscience and Remote Sensing Symposium, 2019Using the long-swath ENVISAT/ASAR acquisitions from 2003 to 2011, we researched evolution characteristics of the postseismic deformation of two strong earthquakes in the northern part of the Tibet Plateau in the past 20 years, namely the 1997 Mw7.6 Manyi Earthquake and the 2001 Ms8.1 Kokoxili earthquake.
Chunyan Qu +3 more
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