Results 81 to 90 of about 468 (176)
Interseismic deformation in the Nepal Himalaya from GPS data
The velocity of interseismic convergence through the Nepal Himalaya - essential parameter in the study of the seismic cycle - is discussed since several years. To constrain this velocity, we have successfully combined geodetic data from campaign GPS surveys, cGPS stations and DORIS stations to determine the plate motion of India and contemporary ...
openaire +1 more source
The relationships between co-seismic slip and surface deformation under different rupture patterns along the Main Himalayan Thrust remain poorly understood.
Chong Yue +6 more
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Interseismic deformation fingerprints on the hyperarid coastal landscape in North Chilean subduction
Along-strike seismotectonic behavior of subduction megathrusts feeds back into the forearc deformation as elastic and permanent deformation. However, whether and how short-term elastic deformation reflects long-term permanent deformation in the forearc and shapes the coastal region remains unclear.
Ehsan Kosari +5 more
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Megaearthquakes (Mw > 8) cause continental-scale, long-lasting surface deformation, mainly due to viscoelastic relaxation of the asthenosphere. To investigate the links between this deformation and the slip history along subduction interfaces—including ...
Hugo Boulze +5 more
doaj +1 more source
AbstractThe seismic hazard along the Himalayan arc remains a focus of discussion due to its huge potential societal impact. Taking advantage of modern, dense geodetic observations, several attempts have been made to provide a clear picture of the present‐day rate of strain accumulation caused by interseismic coupling on the Main Himalayan Thrust (MHT).
Dibyashakti Panda, Eric O. Lindsey
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In the subduction zone of the Kamchatka Peninsula, where the powerful earthquake (Mw 8.2–8.8) of July 29, 2025, repeated the hypocenter location of the 1952 event, the task of studying the spatial heterogeneity of interseismic deformation as an indicator
Bondur Valeriy +4 more
doaj +1 more source
We use recently compiled GNSS velocities across the Zemuhe‐Daliangshan fault zone, part of the central Xianshuihe‐Xiaojiang fault system, to reconcile a long‐standing mismatch between geodetic and geologic slip‐rate estimates.
X. Rui, E. O. Lindsey
doaj +1 more source
Fast relocking and afterslip-seismicity evolution following the 2015 Mw 8.3 Illapel earthquake in Chile. [PDF]
Hormazábal J +9 more
europepmc +1 more source
Interseismic deformation in south‐central Tibet from InSAR and GPS data [PDF]
Hua Wang +3 more
openaire +1 more source
Feedback between megathrust earthquake cycle and plate convergence. [PDF]
Martin de Blas J +3 more
europepmc +1 more source

