Results 1 to 10 of about 5,597 (117)
Imaging evolution of Cascadia slow-slip event using high-rate GPS [PDF]
Scientific Reports, 2022 The slip history of short-term slow slip event (SSE) is typically inferred from daily Global Positioning System (GPS) data, which, however, cannot image the sub-daily processes, leaving the underlying mechanisms of SSEs elusive.
Yuji Itoh, Yosuke Aoki, Junichi Fukuda
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Spatiotemporal slip distributions associated with the 2018–2019 Bungo Channel long-term slow slip event inverted from GNSS data [PDF]
Scientific Reports, 2022 Long-term slow slip events (L-SSEs) have repeatedly occurred beneath the Bungo Channel in southwestern Japan with durations of several months to a couple of years, with a recurrence interval of approximately 6 years.
Yukinari Seshimo, Shoichi Yoshioka
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Secondary acceleration of slip fronts driven by slow slip event coalescence in subduction zones [PDF]
Nature CommunicationsThe coalescence of slow slip events (SSEs) in subduction zones has been proposed as a potential precursor to large earthquakes, yet the physical conditions under which SSE fronts coalesce remain poorly understood.
Ji Wang +7 more
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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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Systematic Detection of Short‐Term Slow Slip Events in Southcentral Alaska
Geophysical Research Letters, 2023 Slow slip events (SSEs) are important for the slip budget along a megathrust fault. Although the recurrence of weeks‐long short‐term SSEs (S‐SSEs) in southcentral Alaska has been suggested, a large amount of noise prevented us from detecting discrete ...
Yutaro Okada, Takuya Nishimura
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Geochemistry, Geophysics, Geosystems, 2020 The month‐to‐year‐long deformation of the Earth's crust where active subduction zones terminate is poorly explored. Here we report on a multidisciplinary data set that captures the synergy of slow‐slip events, earthquake swarms and fault interactions ...
Vasiliki Mouslopoulou +7 more
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Earth, Planets and Space, 2022 Using global navigation satellite system (GNSS) data to detect millimeter-order signals of short-term slow slip events (S-SSEs) and to estimate their source parameters, especially duration, is challenging because of low signal-to-noise ratio.
Yutaro Okada +4 more
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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
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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
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Geophysical Research Letters, 2023 Using new continuous geodetic time series, we identify five shallow slow slip events (SSEs) offshore and beneath the Osa peninsula in southern Costa Rica. An early event was detected by one station in 2013, and two events occurring in close succession in
Mason Perry +4 more
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