Results 201 to 210 of about 1,088,999 (248)
Some of the next articles are maybe not open access.
Postseismic deformation following the 1906 San Francisco earthquake
Journal of Geophysical Research: Solid Earth, 2000We have reevaluated triangulation data from northern California following the 1906 San Francisco earthquake, thereby increasing the temporal and spatial resolution of postseismic deformation following that event. We have calculated uniform shear strain rates and average station velocities at Point Arena using data from 1906–1907, 1929–1930, and 1973 ...
Shelley J. Kenner, Paul Segall
openaire +1 more source
A plate flexure approximation to postseismic and interseismic deformation
Journal of Geophysical Research: Solid Earth, 1985The rather large postseismic deformation that is associated with two‐dimensional dip‐slip faulting in the lithosphere is related to the bending of a free plate generated by dip‐slip faulting. In the absence of gravity, asthenosphere relaxation eventually permits the faulted lithosphere to assume the dihedral configuration of a faulted free plate.
J. C. Savage, Guohua Gu
openaire +1 more source
Coseismic and Early Postseismic Deformation Due to the 2021 M7.4 Maduo (China) Earthquake
, 2021The 2021 Maduo earthquake ruptured a 150 km‐long left‐lateral fault in the northeast Tibet. We used Synthetic Aperture Radar data collected by the Sentinel‐1A/B satellites within days of the earthquake to derive a finite fault model and investigate the ...
Y. Fialko, Zeyu Jin
semanticscholar +1 more source
Journal of Geophysical Research: Solid Earth, 2021
Postseismic deformation following great subduction earthquakes is commonly modeled as the sum of the contributions from afterslip on the megathrust and viscoelastic relaxation of the coseismic stress changes in the mantle.
J. Fukuda, K. Johnson
semanticscholar +1 more source
Postseismic deformation following great subduction earthquakes is commonly modeled as the sum of the contributions from afterslip on the megathrust and viscoelastic relaxation of the coseismic stress changes in the mantle.
J. Fukuda, K. Johnson
semanticscholar +1 more source
Interpretation of postseismic deformation with a viscoelastic relaxation model
Journal of Geophysical Research: Solid Earth, 1980Aleutian tide gages registered coseismic subsidence of 10–15 cm at three locations during the great earthquakes of 1957 and 1965. For approximately 5–6 years after this initial subsidence the data indicate postseismic uplift of the islands to approximately their initial level.
J. Wahr, M. Wyss
openaire +1 more source
Spherical versus flat models of coseismic and postseismic deformations
Journal of Geophysical Research: Solid Earth, 1999We perform an exhaustive study of coseismic and postseismic surface deformations induced by shear dislocations using flat and spherical Earth models. Our aim is to examine the effects of the spherical geometry, the vertical layering, and the self‐gravitation on surface displacement field.
C. Nostro +3 more
openaire +1 more source
Geophysical Journal International
Geodetic observations of postseismic deformation due to afterslip and viscoelastic relaxation can be used to infer fault and lithosphere rheologies by combining the observations with mechanical models of postseismic processes.
J. Fukuda, S. Barbot
semanticscholar +1 more source
Geodetic observations of postseismic deformation due to afterslip and viscoelastic relaxation can be used to infer fault and lithosphere rheologies by combining the observations with mechanical models of postseismic processes.
J. Fukuda, S. Barbot
semanticscholar +1 more source
Journal of Applied Geodesy, 2022
We analyze the Global Positioning System (GPS)-derived strain rate distribution to investigate active crustal structure in Central Java, Indonesia, using ten years (2010–2019) continuous and permanent observation data.
C. Pratama +8 more
semanticscholar +1 more source
We analyze the Global Positioning System (GPS)-derived strain rate distribution to investigate active crustal structure in Central Java, Indonesia, using ten years (2010–2019) continuous and permanent observation data.
C. Pratama +8 more
semanticscholar +1 more source
Journal of Geophysical Research: Solid Earth
In contrast to strong orogenic uplift at the forefront of the Tian Shan belt, the tectonic deformation in its interior is low‐rate, and how it is accommodated remains poorly understood.
P. He +4 more
semanticscholar +1 more source
In contrast to strong orogenic uplift at the forefront of the Tian Shan belt, the tectonic deformation in its interior is low‐rate, and how it is accommodated remains poorly understood.
P. He +4 more
semanticscholar +1 more source
Journal of Geophysical Research: Solid Earth, 2021
Observations of ∼7 years of postseismic deformation following the 2012 M w 7.8 Haida Gwaii and 2013 M w 7.5 Craig earthquakes in western British Columbia and southeastern Alaska provides insight into the regional rheologic structure and seismological ...
Zhen Tian, J. Freymueller, Zhiqiang Yang
semanticscholar +1 more source
Observations of ∼7 years of postseismic deformation following the 2012 M w 7.8 Haida Gwaii and 2013 M w 7.5 Craig earthquakes in western British Columbia and southeastern Alaska provides insight into the regional rheologic structure and seismological ...
Zhen Tian, J. Freymueller, Zhiqiang Yang
semanticscholar +1 more source