Shallow geological structures triggered during the Mw 6.4 Meinong earthquake, southwestern Taiwan
The Meinong earthquake generated up to ~10 cm surface displacement located 10 - 35 km west of the epicenter and monitored by InSAR and GPS. In addition to coseismic deformation related to the deep earthquake source, InSAR revealed three sharp surface ...
Maryline Le Béon +10 more
doaj +1 more source
Interseismic Deformation and Earthquake Hazard along the Southernmost Longitudinal Valley Fault, Eastern Taiwan [PDF]
About half of the 8 cm/yr of oblique convergence across the active convergent plate boundaries of Taiwan occurs in eastern Taiwan, across the Longitudinal Valley. Significant shortening and left‐lateral slip occurs across the Longitudinal Valley fault there, both as shallow fault creep and as seismogenic fault slip.
Chuang, Ray Y. +8 more
openaire +3 more sources
Competing Effects of Elastic Heterogeneity and Viscous Flow on Interseismic Coupling at Cascadia
Interseismic coupling maps are important tools for estimating future earthquake hazard at subduction zones. Often interseismic coupling is estimated from surface velocities using a homogeneous elastic Earth model.
E. M. Sherrill +2 more
doaj +1 more source
Central Sumatra, Indonesia, is historically known for its significant seismic activities, most notably the devastating 1883 earthquake. In this study, we measured the interseismic deformation using continuous GNSS observation data for three years from ...
Ongky Anggara +4 more
doaj +1 more source
Constraints on the Geometry and Frictional Properties of the Main Himalayan Thrust Using Coseismic, Postseismic, and Interseismic Deformation in Nepal [PDF]
The geometry and frictional properties of a fault system are key parameters required to understand its seismic behavior. The Main Himalayan Thrust in Nepal is the type example of a continental megathrust and forms part of a fault system which ...
Elliott, JR +9 more
core +1 more source
Unraveling the surface deformation and fault kinematics during the seismic cycle is crucial for understanding earthquake physics. Herein, we use geodetic and seismic observations to quantify the interseismic coupling, coseismic rupture, and postseismic ...
Yang Xiao +8 more
doaj +1 more source
Models of interseismic deformation with an analytic framework for the inclusion of general linear viscoelastic rheologies [PDF]
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2006.Includes bibliographical references.I investigate postseismic and interseismic deformation using two-dimensional models of a vertical strike-
Hetland, Eric Andreas
core
Residual polar motion caused by coseismic and interseismic deformations from 1900 to present [PDF]
We challenge the perspective that seismicity could contribute to polar motion by arguing quantitatively that, in first approximation and on the average, interseismic deformations can compensate for it. This point is important because what we must simulate and observe in Earth Orientation Parameter time-series over intermediate timescales of decades or ...
G. Cambiotti +3 more
openaire +2 more sources
Pseudotachylytes and cataclasites record transient seismic slips within the brittle–ductile transition zone and ductile flow layers. Investigating the mechanisms of pseudotachylytes can provide the most direct geological evidence for revealing seismic ...
Wenhao Dai +7 more
doaj +1 more source
Slip complementarity and deficit of the East Anatolian Fault revealed by geodetic observations
Catastrophic earthquakes have struck along the East Anatolian Fault (EAF), including the 2020 Elaziğ earthquake and the 2023 Kahramanmaraş earthquake doublet.
Bingquan Han +7 more
doaj +1 more source

