Results 261 to 270 of about 882,743 (301)
Focal mechanism variations reveal mechanical controls on segmentation at oceanic transform faults. [PDF]
Tan F +4 more
europepmc +1 more source
Off-fault damage controls near-surface rupture behaviour in soft sediments. [PDF]
De Paola N +4 more
europepmc +1 more source
Probing Slow Earthquakes With Deep Learning [PDF]
AbstractSlow earthquakes may trigger failure on neighboring locked faults that are stressed sufficiently to break, and slow slip patterns may evolve before a nearby great earthquake. However, even in the clearest cases such as Cascadia, slow earthquakes and associated tremor have only been observed in intermittent and discrete bursts.
Ian W McBrearty +2 more
exaly +5 more sources
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Connecting slow earthquakes to huge earthquakes
Science, 2016Slow earthquakes are characterized by a wide spectrum of fault slip behaviors and seismic radiation patterns that differ from those of traditional earthquakes. However, slow earthquakes and huge megathrust earthquakes can have common slip mechanisms and are located in neighboring regions of the seismogenic zone.
Aitaro Kato, Kazushige Obara
exaly +3 more sources
Slow earthquakes triggered by typhoons
Nature, 2009The first reports on a slow earthquake were for an event in the Izu peninsula, Japan, on an intraplate, seismically active fault. Since then, many slow earthquakes have been detected. It has been suggested that the slow events may trigger ordinary earthquakes (in a context supported by numerical modelling), but their broader significance in terms of ...
ChiChing, Liu +2 more
openaire +2 more sources
A scaling law for slow earthquakes
Nature, 2007Recently, a series of unusual earthquake phenomena have been discovered, including deep episodic tremor, low-frequency earthquakes, very-low-frequency earthquakes, slow slip events and silent earthquakes. Each of these has been demonstrated to arise from shear slip, just as do regular earthquakes, but with longer characteristic durations and radiating ...
Satoshi, Ide +3 more
openaire +2 more sources
Slow earthquakes and great earthquakes along the Nankai trough
Earth and Planetary Science Letters, 2002Abstract We have reexamined reports indicating that slow deformation occurred before the great Japan earthquakes of 1944 (Tonankai) and 1946 (Nankaido) and find that the observations are well founded. Although no quantitative models have previously been proposed to explain all of the relevant data we show that they are satisfied by a simple model for
Alan T Linde
exaly +2 more sources
Slow Earthquakes Coincident with Episodic Tremors and Slow Slip Events
Science, 2007We report on the very-low-frequency earthquakes occurring in the transition zone of the subducting plate interface along the Nankai subduction zone in southwest Japan. Seismic waves generated by very-low-frequency earthquakes with seismic moment magnitudes of 3.1 to 3.5 predominantly show a long period of about 20 seconds.
Yoshihiro, Ito +4 more
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Towards Slow Earthquakes Forecasting
2020<p>Slow Slip Events (SSEs) are episodic slip events that play a significant role in the moment budget along subduction megathrust. They share many similarities with regular earthquakes, and have been observed in major subduction regions like, for example, Cascadia, Japan, Mexico, New Zealand.
Adriano Gualandi +3 more
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A Brownian walk model for slow earthquakes [PDF]
Along some subduction plate boundaries, slow deformation is observable as seismically detected deep low‐frequency tremor and geodetically detected slow slip events. These phenomena are considered as different manifestations of slow earthquakes characterized by fairly constant seismic moment rate.
Satoshi Ide
exaly +2 more sources

