Results 151 to 160 of about 468 (176)
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Tectonophysics, 2013
Abstract We make use of two-step modeling to simulate inter- and coseismic deformation within one seismic cycle by means of visco-elastic finite element method (FEM). The first step is to perform inversion to find the optimum modeling parameters by fitting the observed interseismic deformation.
Shoubiao Zhu, Peizhen Zhang
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Abstract We make use of two-step modeling to simulate inter- and coseismic deformation within one seismic cycle by means of visco-elastic finite element method (FEM). The first step is to perform inversion to find the optimum modeling parameters by fitting the observed interseismic deformation.
Shoubiao Zhu, Peizhen Zhang
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Diffuse interseismic deformation across the Pacific–North America plate boundary
Geology, 2007Crustal movements and deformation within the diffuse Pacifi c‐North America (Pa-NA) plate boundary are dominated by the right-lateral motion between the two plates. By using the Pa-NA pole of rotation (PoR) spherical coordinate system, we decompose observed crustal movements into parallel and normal components to the Pa-NA plate motion.
Shimon Wdowinski +3 more
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2023
We present a comprehensive analysis of geodetic data, including InSAR imagery and GNSS observations, to assess the pattern of ground motions of the Paliki peninsula in western Cephalonia, Greece. Paliki is prone to frequent, strong earthquakes, due to its close proximity to the right-lateral Cephalonia Transform Fault (CTF), a 140 km long strike-slip ...
Tsironi, V. +6 more
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We present a comprehensive analysis of geodetic data, including InSAR imagery and GNSS observations, to assess the pattern of ground motions of the Paliki peninsula in western Cephalonia, Greece. Paliki is prone to frequent, strong earthquakes, due to its close proximity to the right-lateral Cephalonia Transform Fault (CTF), a 140 km long strike-slip ...
Tsironi, V. +6 more
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Tectonophysics, 2013
Abstract The deformations of the overriding and subducting plates during the seismic cycle associated with large subduction earthquakes are modelled using 2D and 3D finite element techniques. A particular emphasis is put on the interseismic velocities and on the impact of the rheology of the asthenosphere.
Olga Trubienko +3 more
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Abstract The deformations of the overriding and subducting plates during the seismic cycle associated with large subduction earthquakes are modelled using 2D and 3D finite element techniques. A particular emphasis is put on the interseismic velocities and on the impact of the rheology of the asthenosphere.
Olga Trubienko +3 more
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Kinematic models of interseismic deformation in Southern California
2004We develop a framework for interpreting geodetic measurements of interseismic deformation and geologic slip rate estimates in terms of block motions. This method accounts for the effects of block rotations and interseismic strain accumulation from active fults. We find that the San Andreas Fault slips close to Its Holocene rate in the Carrizo Plain (35.
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IMPORTANCE OF VISCOELASTIC STRESS RELAXATION IN BOTH POSTSEISMIC AND INTERSEISMIC DEFORMATION
Geological Society of America Abstracts with Programs, 2017Kelin Wang, Tianhaozhe Sun, Shaoyang Li
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