Results 31 to 40 of about 9,671 (264)
Slow Slip Event at Kilauea Volcano [PDF]
Eos, Transactions American Geophysical Union, 2010 Early in the morning of 1 February 2010 (UTC; early afternoon 31 January 2010 local time), continuous Global Positioning System (GPS) and tilt instruments detected a slow slip event (SSE) on the south flank of Kilauea volcano, Hawaii. The SSE lasted at least 36 hours and resulted in a maximum of about 3 centimeters of seaward displacement.
Michael Poland +10 more
openaire +1 more source
Geophysical Research Letters, 2023 Recent observations beneath central Japan have shown that periodic fluid drainage occurs during slow‐slip events (SSEs) based on temporal variations in QP−1 above the megathrust boundary of the subducting Philippine Sea slab. However, no previous studies
Yosuke Ito, Junichi Nakajima
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
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Estimating the occurrence of slow slip events and earthquakes with an ensemble Kalman filter [PDF]
, 2023 Our ability to forecast earthquakes and slow slip events is hampered by limited information on the current state of stress on faults. Ensemble data assimilation methods permit estimating the state by combining physics-based models and observations, while
Diab Montero, H.A. +7 more
core +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
Revealing the cluster of slow transients behind a large slow slip event [PDF]
Science Advances, 2018 A slow slip event is a cluster of small aseismic slip transients intermittently interrupted by relocking of the plate interface.
Frank, William +3 more
openaire +5 more sources
Geochemistry, Geophysics, Geosystems, 2023 Slow slip events in the northern Hikurangi margin of Aotearoa New Zealand occur every 18–24 months and last for several weeks before returning to average convergence rates of around 38 mm/yr.
Jefferson Yarce +2 more
doaj +1 more source
Frontiers in Earth Science, 2022 The southernmost Ryukyu subduction zone may have a geodetically inferred Mw 7.5 to 8.7 megathrust earthquake in a shallow locked region, the Ryukyu fault.
Sean Kuanhsiang Chen +4 more
doaj +1 more source
Transient Slow Slip Characteristics of Frictional‐Viscous Subduction Megathrust Shear Zones
AGU Advances, 2021 The deep roots of subduction megathrusts exhibit aseismic slow slip events, commonly accompanied by tectonic tremor. Observations from exhumed rocks suggest this region of the subduction interface is a shear zone with frictional lenses embedded in a ...
Whitney M. Behr +3 more
doaj +1 more source
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