Results 31 to 40 of about 110,973 (285)
Slow slip events are regular earthquakes [PDF]
Abstract Slow slip events usually occur downdip of seismogenic zones in subduction megathrusts and crustal faults, with rupture speeds much slower than earthquakes. The empirical moment-duration scaling relation can help constrain the physical mechanism of slow slip events, yet it is still debated whether this scaling is linear or cubic and a ...
openaire +2 more sources
Integrated rupture mechanics for slow slip events and earthquakes
AbstractSlow slip events occur worldwide and could trigger devastating earthquakes, yet it is still debated whether their moment-duration scaling is linear or cubic and a fundamental model unifying slow and fast earthquakes is still lacking. Here, we show that the rupture propagation of simulated slow and fast earthquakes can be predicted by a newly ...
Weng, Huihui, Ampuero, Jean-Paul
openaire +4 more sources
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
doaj +1 more source
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
doaj +1 more source
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
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
doaj +1 more source
Recovery of the recurrence interval of Boso slow slip events in Japan
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
Slow slip events in the roots of the San Andreas fault [PDF]
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
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
Imaging of the early acceleration phase of the 2013–2014 Boso slow slip event
Junichi Fukuda, Aitaro Kato
exaly +2 more sources

