Seismic evidence for lower-mantle heat supply beneath the Cordilleran slab window in western Canada. [PDF]
Zhang Q, Audet P, Ji C, Estève C.
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Sluggish post-garnet transformation controls slab stagnation at the uppermost lower mantle. [PDF]
Shen Y, Yang J, Zhao L.
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Late Quaternary activities of the Xinbaoan-Shacheng fault in the North China Plain. [PDF]
Qiu C +6 more
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Mitigation Strategies for Long-Term Corrosion in CFST Structures: A Systematic Review. [PDF]
Alsafi S +4 more
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Advanced single-strut modelling of lightweight in-filled RC frames: validation and seismic performance assessment. [PDF]
El-Fotuh GA, Attia WA, El-Feky MS.
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Geodetic Constraints on Segment-Scale Slip Rates and Interseismic Coupling Along the Havran-Balıkesir Fault Zone, NW Anatolia, Türkiye. [PDF]
Tiryakioğlu İ +12 more
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Structural and stratigraphic controls on reservoir distribution in the Ptah oil field, Shushan Basin, North Western Desert, Egypt. [PDF]
Shamia KES, Othman AAA, Fathy M.
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Shaking table model test and numerical analysis of the steeply dipping bedded rock slopes under seismic actions. [PDF]
Wang C +5 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 ...
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Post-seismic viscoelastic deformation
The 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 ...
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