Postglacial rebound at the northern Cascadia subduction zone
Postglacial rebound is the response of the Earth to the decay of ice-sheets. A postglacial
rebound model explains crustal tilting and rapid uplift at the northern Cascadia subduction …
rebound model explains crustal tilting and rapid uplift at the northern Cascadia subduction …
[图书][B] Global dynamics of the Earth
R Sabadini, B Vermeersen, G Cambiotti - 2016 - Springer
With this book we provide graduate students with the mathematical techniques necessary to
solve some basic problems related to the deformation of the Earth by a variety of …
solve some basic problems related to the deformation of the Earth by a variety of …
Afterslip and viscoelastic relaxation following the 2011 Tohoku‐oki earthquake (Mw9.0) inferred from inland GPS and seafloor GPS/Acoustic data
S Yamagiwa, S Miyazaki, K Hirahara… - Geophysical …, 2015 - Wiley Online Library
We simultaneously estimate 2.5 years of afterslip and viscoelastic relaxation, as well as
coseismic slip, for the 2011 Tohoku‐oki earthquake. Displacements at inland GPS and …
coseismic slip, for the 2011 Tohoku‐oki earthquake. Displacements at inland GPS and …
Temporal change of interplate coupling in northeastern Japan during 1995–2002 estimated from continuous GPS observations
T Nishimura, T Hirasawa, S Miyazaki… - Geophysical Journal …, 2004 - academic.oup.com
Temporal change of deformation in northeastern Japan is clarified by continuous Global
Positioning System (GPS) observations from 1995 April to 2002 March. The observed GPS …
Positioning System (GPS) observations from 1995 April to 2002 March. The observed GPS …
Overlapping post-seismic deformation processes: afterslip and viscoelastic relaxation following the 2011 Mw 9.0 Tohoku (Japan) earthquake
Large tectonic earthquakes lead to significant deformations in the months and years
thereafter. These so-called post-seismic deformations include contributions mainly from …
thereafter. These so-called post-seismic deformations include contributions mainly from …
Bayesian Inversion for a Stress‐Driven Model of Afterslip and Viscoelastic Relaxation: Method and Application to Postseismic Deformation Following the 2011 MW …
J Fukuda, KM Johnson - Journal of Geophysical Research …, 2021 - Wiley Online Library
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 sum of the contributions from afterslip on the megathrust and viscoelastic relaxation of …
FEM simulation of interseismic and coseismic deformation associated with the 2008 Wenchuan Earthquake
S Zhu, P Zhang - Tectonophysics, 2013 - Elsevier
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 …
seismic cycle by means of visco-elastic finite element method (FEM). The first step is to …
[HTML][HTML] 青藏高原东北缘地震时空迁移的有限元数值模拟
孙云强， 罗纲 - 地球物理学报, 2018 - html.rhhz.net
地震在大陆内部断层系统中的时空迁移和丛集的基本力学机制一直是地球科学家关注的重要
问题. 青藏高原东北缘地震活动频繁, 其地震时空迁移和地震丛集现象显著 …
问题. 青藏高原东北缘地震活动频繁, 其地震时空迁移和地震丛集现象显著 …
Elastic and viscoelastic models of crustal deformation in subduction earthquake cycles
K Wang - The seismogenic zone of subduction thrust faults, 2007 - degruyter.com
An ideal model of subduction earthquake cycles that includes tectonic loading, rate-
dependent friction, and viscoelastic stress relaxation is not yet available. For comparison …
dependent friction, and viscoelastic stress relaxation is not yet available. For comparison …
Importance of rheological heterogeneity for interpreting viscoelastic relaxation caused by the 2011 Tohoku-Oki earthquake
H Suito - Earth, Planets and Space, 2017 - Springer
This study develops a three-dimensional viscoelastic model using the finite element method
to understand the postseismic deformation that followed the 2011 Tohoku-Oki earthquake …
to understand the postseismic deformation that followed the 2011 Tohoku-Oki earthquake …