Results 231 to 240 of about 5,589,742 (255)
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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
openaire +1 more source
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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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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Post-seismic Deformation Monitoring With The COSMO/SKYMED Constellation
2011COSMO/SKYMED is currently the unique constellation of synthetic aperture radar (SAR) sensors operative, which is also for civilian use. On April 6, 2009, an Mw 6.3 earthquake struck the city of lAquila in Central Italy. The constellation acquired data stacks over the hit area at an unprecedented temporal rate.
D Reale +5 more
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Andaman post-seismic deformation observations: An update
2009Paul, John, , Rajendran, Lowry A
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Evaluation of Post-Seismic Ground Deformation Using the D-InSAR Technique
2021Bijay Halder +3 more
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Frictional Strength of Faults: Evidence for Post Seismic Deformation
10th Congress of the Balkan Geophysical Society, 2019openaire +1 more source