Results 21 to 30 of about 25,655 (271)
Slow slip events in the roots of the San Andreas fault. [PDF]
Sci Adv, 2019 By analyzing GPS time series, we have detected an averaged M w 4.9 slow slip event in the roots of the San Andreas fault.
Rousset B, Bürgmann R, Campillo M.
europepmc +6 more sources
What’s down there? The structures, materials and environment of deep-seated slow slip and tremor [PDF]
Philosophical Transactions Series A, Mathematical, Physical, and Engineering Sciences, 2021 Whitney M Bèhr, Roland Burgmann
exaly +2 more sources
Geophysical Research LettersLike earthquakes, slow slip events release elastic energy stored on faults. Yet, the mechanisms behind slow slip instability and its relationship with seismicity are debated. Here, we use a seismo‐geodetic deployment to document a shallow slow slip event
Jannes Münchmeyer +8 more
doaj +2 more sources
Slow-slip events in semi-brittle serpentinite fault zones. [PDF]
Sci Rep, 2018 Slow-slip events are earthquake-like events only with much lower slip rates. While peak coseismic velocities can reach tens of meters per second, slow-slip is on the order of 1E-7 m/s and may last for days to weeks.
Goswami A, Barbot S.
europepmc +5 more sources
Origin of slow earthquake statistics in low-friction soft granular shear [PDF]
Nature CommunicationsSlow earthquakes differ from regular earthquakes in their slower moment release and size distribution dominated by smaller events. However, the physical origin of these slow earthquake statistics remains controversial.
Yuto Sasaki, Hiroaki Katsuragi
doaj +2 more sources
Slow slip events following the afterslip of the 2002 Mw 7.1 Hualien offshore earthquake, Taiwan
Earth, Planets and Space, 2022 Geodetic evidence for slow slip recurrence changed by stress perturbations was rare, especially from afterslip following a nearby large earthquake. The first observed slow slip events in the southernmost Ryukyu subduction had occurred in 2005, 2009, and ...
Sean Kuanhsiang Chen +2 more
doaj +1 more source
Precursory Slow Slip and Foreshocks on Rough Faults [PDF]
Journal of Geophysical Research: Solid Earth, 2020 AbstractForeshocks are not uncommon prior to large earthquakes, but their physical mechanism remains controversial. Two interpretations have been advanced: (1) foreshocks are driven by aseismic nucleation and (2) foreshocks are cascades, with each event triggered by earlier ones.
Camilla Cattania, Paul Segall
openaire +3 more sources
Geophysical Research Letters, 2022 Earthquakes and slow‐slip events interact, however, detailed studies investigating their interplay are still limited. We generate the highest resolution microseismicity catalog to date for the northern Armutlu Peninsula in a ∼1‐year period to perform a ...
G. M. Bocchini +6 more
doaj +1 more source
Filling the Gap in Cascadia: The Emergence of Low‐Amplitude Long‐Term Slow Slip
Geochemistry, Geophysics, Geosystems, 2021 Long‐term slow slip events have been observed at several subduction zones around the globe, where they play an integral part in strain release along megathrust faults.
Carolyn P. Nuyen, David A. Schmidt
doaj +1 more source
Quake clamps down on slow slip [PDF]
Geophysical Research Letters, 2014 AbstractUsing continuous GPS (cGPS) data from the Hikurangi subduction zone in New Zealand, we show for the first time that stress changes induced by a local earthquake can arrest an ongoing slow slip event (SSE). The cGPS data show that the slip rate in the northern portion of the 2013/2014 Kapiti SSE decreased abruptly following a nearby intraslab ...
Laura M. Wallace +3 more
openaire +3 more sources