Results 261 to 270 of about 147,471 (299)
A mixture design approach of hydraulic asphalt concrete considering regional deformation characteristics. [PDF]
Sci RepLi H, He J, Liu L.
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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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Advances in Space Research, 2021
On January 21, 2016, a Mw 5.9 earthquake occurred in Menyuan, Qinghai Province, in northwestern China, which is an earthquake-prone region located along the northeastern margin of the Tibetan Plateau. However, the source parameters, deformation mechanism,
W. Qu +6 more
semanticscholar +3 more sources
On January 21, 2016, a Mw 5.9 earthquake occurred in Menyuan, Qinghai Province, in northwestern China, which is an earthquake-prone region located along the northeastern margin of the Tibetan Plateau. However, the source parameters, deformation mechanism,
W. Qu +6 more
semanticscholar +3 more sources
Quantification and modelling of post-seismic deformation following the 24 September 2013 Mw 7.7 earthquake in the Makran region, Pakistan [PDF]
Geophysical Journal International, 2022 On 24 September 2013, an earthquake of magnitude Mw 7.7 occurred on the Hoshab fault in southern Pakistan, south of the 650-km-long Chaman Fault, within the eastern Makran accretionary wedge.
P. Bascou, F. Jouanne
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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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Geophysical Journal International, 2023
The objective of this study was to examine co- and post-seismic deformation following the 2011 Mw9.0 Tohoku-Oki earthquake and its impact on Northeast Asia.
Tai Liu +9 more
semanticscholar +1 more source
The objective of this study was to examine co- and post-seismic deformation following the 2011 Mw9.0 Tohoku-Oki earthquake and its impact on Northeast Asia.
Tai Liu +9 more
semanticscholar +1 more source
Toroidal/poloidal partitioning of global post-seismic deformation
Geophysical Research Letters, 1995 An Earth model subject to dislocations is studied in order to investigate the toroidal/poloidal content of global post‐seismic deformation. Differently from previous analyses, our approach allows us to deal with some of the main complexities of the real Earth, such as sphericity, self‐gravitation, and rheological stratification.
R. Sabadini, A. Piersanti, G. Spada
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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.
R. Sabadini, B. Vermeersen, G. Cambiotti
semanticscholar +2 more sources
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.
R. Sabadini, B. Vermeersen, G. Cambiotti
semanticscholar +2 more sources
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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