Results 61 to 70 of about 4,021 (150)
Shallow Creep in the Leaky Stress Shadow of Locked Zones of Subduction Megathrust
In some subduction zones such as Nankai, creeping of the shallow part of the megathrust in the stress shadow of deeper locked zones is detected by seafloor geodetic measurements and/or reflected by slow earthquakes (SEQs).
Kelin Wang, Yajing Liu, Tianhaozhe Sun
doaj +1 more source
Relative plate motion in subduction zones transitions from frictional slip to viscous flow with increasing depth and temperature. The frictional‐viscous transition can control the depth extent of megathrust earthquakes and episodic tremor and slip (ETS).
So Ozawa +2 more
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Recently, integrated geophysical‐geological surveys in the Nankai subduction zone in Japan have revealed that slow earthquakes repeatedly occur beneath the outer wedge of the forearc.
G. Kimura +6 more
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SLOW EARTHQUAKES IN CENTRAL ITALY
[1] Slow earthquakes and afterslips prove that the Earth does not have just two response time scales, i.e. that of tectonic loading and that of regular earthquakes. A swarm of slow earthquakes, with time constants of the order of hundreds of seconds, has been detected by a laser interferometer below the Gran Sasso massif (Italy).
Andrea Morelli +3 more
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Connecting slow earthquakes to huge earthquakes
UTokyo Research掲載「スロー地震の巨大地震との関連性」 URI: http://www.u-tokyo.ac.jp/ja/utokyo-research/research-news/connecting-slow-earthquakes-to-huge-earthquakes.html UTokyo Research "Connecting slow earthquakes to huge earthquakes" URI: http://www.u-tokyo.ac.jp/en/utokyo-research/research-news/connecting-slow-earthquakes-to-huge-earthquakes ...
openaire
Development of a Slow Earthquake Database
identifier:oai:t2r2.star.titech.ac.jp ...
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On 9 November 2025, a Mw 6.8 Sanriku‐Oki earthquake struck a Japan Trench segment with inferred recurrent aseismic slip and Mw ∼7 earthquakes. Using S‐net seafloor data, we examine the preparatory and post‐mainshock evolution of this foreshock–mainshock ...
Keisuke Yoshida
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Since their discovery over 25 years ago, slow slip events (SSEs) have been regarded as key phenomena for better understanding the characteristics and kinematics of faults.
Yutaro Okada, Takuya Nishimura
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Abundant fluids in southern Kumano Basin linked to fluid source and slow earthquakes at the plate boundary in the Nankai Trough. [PDF]
Liu X +6 more
europepmc +1 more source
Frictional instabilities in clay illuminate the origin of slow earthquakes. [PDF]
Volpe G +4 more
europepmc +1 more source

