Results 61 to 70 of about 2,530 (204)
Areas prone to slow slip events impede earthquake rupture propagation and promote afterslip. [PDF]
Sci Adv, 2018 Frequent slow slip events and rapid postseismic slip reveal persistent aseismic fault areas delineating future seismic ruptures.
Rolandone F +9 more
europepmc +6 more sources
Dynamics of a velocity strengthening fault region: Implications for slow earthquakes and postseismic slip [PDF]
, 2008 We consider the effect of permanent stress changes on a velocity strengthening rate-and-state fault, through numerical simulations and analytical results on 1-D, 2-D, and 3-D models.
Ampuero, Jean-Paul, Perfettini, Hugo
core +2 more sources
Frontiers in Earth ScienceThe postseismic deformation following the April 2019 Mw 6.2 Hualien earthquake presents an unique opportunity to investigate the mechanisms by which the northern section of the Longitudinal Valley accommodates lithospheric deformation.
Hsiao-Fan Lin +3 more
doaj +1 more source
Geophysical Research Letters, Volume 53, Issue 8, 28 April 2026.Abstract Recent megathrust earthquakes preceded by slow slip events highlight static stress transfer as a key triggering mechanism. However, there are limited insights into the interplay between static stress transfer and elevated fluid pressure before earthquake triggering.
Sean Kuanhsiang Chen +4 more
wiley +1 more source
Geochemistry, Geophysics, Geosystems, 2021 The 2018 Mw7.5 Palu earthquake is a remarkable strike‐slip event due to its nature as a shallow supershear fault rupture across several segments and a destructive tsunami that followed coseismic deformation. GPS offsets in the wake of the 2018 earthquake
N. Nijholt +4 more
doaj +1 more source
Geophysical Research Letters, Volume 53, Issue 8, 28 April 2026.Abstract Large earthquakes can activate complex aftershock fault networks. In such systems, what controls the spatiotemporal evolution of early aftershocks remains a critical yet unresolved problem. Here, using the 2019 M 7.1 Ridgecrest earthquake as an example, we partition the first 10 days of aftershocks onto 15 branching faults activated by the ...
Yanlan Hu, Xin Cui, Zefeng Li
wiley +1 more source
Early aftershocks and afterslip surrounding the 2015 Mw 8.4 Illapel rupture [PDF]
Earth and Planetary Science Letters, 2017 On 16 September 2015, the Mw 8.4 Illapel earthquake ruptured a section of the subduction thrust on the west coast of central Chile. The mainshock was followed by numerous aftershocks including some normal-faulting events near the trench. We apply a template matching approach to improve the completeness of early aftershocks within one month of the ...
Hui Huang +4 more
openaire +3 more sources
Decay and expansion of the early aftershock activity following the 2011 Mw9.0 Tohoku earthquake [PDF]
, 2012 journal ...
Enescu B. +3 more
core +6 more sources
Aftershock production rate of driven viscoelastic interfaces [PDF]
, 2014 We study analytically and by numerical simulations the statistics of the aftershocks generated after large avalanches in models of interface depinning that include viscoelastic relaxation effects.
Jagla, E. A.
core +2 more sources
SeismicaSurface afterslip can persist over several years, with displacements reaching tens of centimeters. Such deformations can damage structures, making it crucial to understand their temporal changes for effective post-earthquake reconstruction.
Yoshiya Iwasa +3 more
doaj +1 more source