Results 21 to 30 of about 172,085 (299)
Slow slip events in the roots of the San Andreas fault [PDF]
Science Advances, 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, Baptiste +2 more
openaire +4 more sources
Slow slip and the transition from fast to slow fronts in the rupture of frictional interfaces [PDF]
, 2014 The failure of the population of micro-junctions forming the frictional interface between two solids is central to fields ranging from biomechanics to seismology. This failure is mediated by the propagation along the interface of various types of rupture
Amundsen, David Skålid +5 more
core +3 more sources
Recovery of the recurrence interval of Boso slow slip events in Japan
Earth, Planets and Space, 2019 We present the spatiotemporal evolution of the Boso slow slip event with a moment of 20 × 1018 N m that occurred in June 2018; such events, which have a duration of 1–2 weeks, have repeatedly occurred off the Boso peninsula, east Japan.
Shinzaburo Ozawa +2 more
doaj +1 more source
Extent and Duration of the 2003 Cascadia Slow Earthquake [PDF]
, 2005 Inversion of continuous GPS measurements from the Pacific Northwest show the 2003 Cascadia slow earthquake to be among the largest of ten transients recognized here. Twelve stations bracketing slow slip indicate transient slip propagated bi-directionally
Altamimi +29 more
core +2 more sources
Variations in slow slip moment rate associated with rapid tremor reversals in Cascadia [PDF]
, 2016 During large slow slip events, tremor sometimes propagates in the reverse along-strike direction for a few hours, at speeds 10 to 40 times faster than the forward propagation.
Bostock, MG +3 more
core +1 more source
Dilatant strengthening as a mechanism for slow slip events [PDF]
Journal of Geophysical Research: Solid Earth, 2010 The mechanics of slow slip events (SSE) in subduction zones remain unresolved. We suggest that SSE nucleate in areas of unstable friction under drained conditions, but as slip accelerates dilatancy reduces pore pressure p quenching instability. Competition between dilatant strengthening and thermal pressurization may control whether slip is slow or ...
Segall, Paul +3 more
openaire +2 more sources
Geoscience Letters, 2023 We used Global Navigation Satellite System (GNSS) time series data to estimate the spatiotemporal slip distribution for a long-term slow slip event (L-SSE) that occurred in the Tokai region, central Japan, from 2012 to 2016.
Yukinari Seshimo +3 more
doaj +1 more source
Convergence rate across the Nepal Himalaya and interseismic coupling on the Main Himalayan Thrust: Implications for seismic hazard [PDF]
, 2012 We document geodetic strain across the Nepal Himalaya using GPS times series from 30 stations in Nepal and southern Tibet, in addition to previously published campaign GPS points and leveling data and determine the pattern of interseismic coupling on the
Ader, Thomas +14 more
core +5 more sources
Very Low Frequency Earthquakes in Between the Seismogenic and Tremor Zones in Cascadia?
AGU Advances, 2022 Megathrust earthquakes and their associated tsunamis cause some of the worst natural disasters. In addition to earthquakes, a wide range of slip behaviors are present at subduction zones, including slow earthquakes that span multiple orders of spatial ...
Wenyuan Fan +6 more
doaj +1 more source
Frontiers in Earth Science, 2021 In our recent study, we detected the pore pressure change due to the slow slip event (SSE) in March 2020 at the two borehole stations (C0002 and C0010), where the other borehole (C0006) close to the Nankai Trough seems not because of instrumental drift ...
Keisuke Ariyoshi +14 more
doaj +1 more source