Results 131 to 140 of about 415 (163)
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Inference of postseismic deformation mechanisms of the 1923 Kanto earthquake
Journal of Geophysical Research: Solid Earth, 2006Coseismic slip associated with the M7.9, 1923 Kanto earthquake is fairly well understood, involving slip of up to 8 m along the Philippine Sea–Honshu interplate boundary under Sagami Bay and its onland extension. Postseismic deformation after the 1923 earthquake, however, is relatively poorly understood.
Fred F. Pollitz +3 more
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Postseismic deformation following the Landers earthquake, California, 28 June 1992
Bulletin of the Seismological Society of America, 1994AbstractAccelerated strain followed the Landers and Big Bear earthquakes, returning to the normal rate only after a period of several months. We observed this strain throughout most of southern California using the Global Positioning System (GPS). Three GPS receivers operating continuously in fixed positions at Pinyon Flat, Jet Propulsion Laboratory ...
Zheng-Kang Shen +6 more
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Short‐time postseismic deformation of 2001 Ms8.1 Kunlun (China) earthquake
Concurrency and Computation: Practice and Experience, 2010AbstractAfter the Ms 8.1 Kunlun earthquake, postseismic displacements were resolved with GPS. The observed data showed that there were significant differences between the deformations on the south and the north sides of the Kunlun fault. In addition, it is shown that the direction of deformation on the north side shifted from westward to eastward after
Shao Zhi‐Gang +2 more
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Postseismic deformation following the 1991 Racha, Georgia earthquake
2006The April 29, 1991 Racha, Georgia Mw=6.9 earthquake was the largest earthquake recorded in the western section of the Greater Caucasus Mountains. Lithospheric deformation following this earthquake was recorded by a network of eight GPS stations. These data were modeled for postseismic deformation with the mechanisms of afterslip and viscoelastic ...
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3D Green's functions for coseismic and postseismic deformation
2018Finite fault slip inversions are constrained by observational data of surface displacement and Green's functions calculated via a forward model of surface deformation. Although observational techniques in space geodesy have improved greatly in recent years, models of earthquake deformation generally do not include realistic Earth structure. Many finite
Langer, L. +3 more
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Journal of Geophysical Research: Solid Earth, 1983
The principal purpose of this paper is to examine whether movement of matter in a stratified viscoelastic earth can enhance the excitation of the Chandler wobble. We have constructed analytically a two‐layer model consisting of an elastic lithosphere overlying a Maxwell viscoelastic mantle in order to calculate explicitly the temporal evolution of the ...
Dragoni M., Yuen D. A., Boschi E.
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The principal purpose of this paper is to examine whether movement of matter in a stratified viscoelastic earth can enhance the excitation of the Chandler wobble. We have constructed analytically a two‐layer model consisting of an elastic lithosphere overlying a Maxwell viscoelastic mantle in order to calculate explicitly the temporal evolution of the ...
Dragoni M., Yuen D. A., Boschi E.
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The vertical postseismic deformation following the 2004 Parkfield earthquake
Studies have shown that the postseismic transient following the 2004 Parkfield earthquake is dominated by aftersllip. However, the studies are mainly focus on the horizontal deformation and ignore the vertical deformation. The focus of this study is the postseismic deformion in vertical caused by 2004 event.Weijie Tan, danan dong, junping Chen
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Integrative oncology: Addressing the global challenges of cancer prevention and treatment
Ca-A Cancer Journal for Clinicians, 2022Jun J Mao,, Msce +2 more
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