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A slow slip event in the south central Alaska Subduction Zone and related seismicity anomaly [PDF]
Author Posting. © American Geophysical Union, 2012. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 39 (2012): L15309,
Meng Wei +2 more
exaly +2 more sources
Silent triggering: Aseismic crustal faulting induced by a subduction slow slip event
Slow Slip Events (SSEs) are a form of fault slip behaviour whose importance has only been recognised in the last decade at subduction zone plate boundaries worldwide.
Ian J Hamling, Laura M Wallace
exaly +2 more sources
In Guerrero, Mexico, slow-slip events have been observed in a seismic gap, where no earthquakes have occurred since 1911. A rupture of the entire gap today could result in a Mw 8.2–8.4 earthquake.
David P S Bekaert +2 more
exaly +1 more source
International audienceWe document a 1 week long slow slip event (SSE) with an equivalent moment magnitude of 6.0-6.3 which occurred in August 2010 below La Plata Island (Ecuador), south of the rupture area of the 1906 Mw= 8.8 megathrust earthquake.
Martin Vallée +2 more
exaly +2 more sources
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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
openaire +2 more sources
Ultralow frictional healing explains recurring slow slip events
Science, 2023Plate motion on shallow subduction megathrusts is accommodated by a spectrum of tectonic slip modes. However, the frictional properties and conditions that sustain these diverse slip behaviors remain enigmatic. Frictional healing is one such property, which describes the degree of fault restrengthening between earthquakes.
Srisharan Shreedharan +3 more
openaire +2 more sources
Seismic evidence of nonlinear crustal deformation during a large slow slip event in Mexico
International audienceRepeated cross-correlations of ambient seismic noise indicate a long-term seismic velocity change associated with the 2006 M7.5 slow-slip event (SSE) in the Guerrero region, Mexico.
Diane Rivet +2 more
exaly +3 more sources
Slow Slip Events in New Zealand
Annual Review of Earth and Planetary Sciences, 2020Continuously operating global positioning system sites in the North Island of New Zealand have revealed a diverse range of slow motion earthquakes on the Hikurangi subduction zone. These slow slip events (SSEs) exhibit diverse characteristics, from shallow (<15 km), short (<1 month), frequent (every 1–2 years) events in the northern part of the ...
openaire +3 more sources
Fault constitutive relations inferred from the 2009‐2010 slow slip event in Guerrero, Mexico [PDF]
The spatiotemporal evolution of stress state is analyzed during the 2009-2010 Slow Slip Event (SSE) of Guerrero, Mexico, based on the kinematic inversion results and using an integral expression for stress changes.
Julie Maury +2 more
exaly +2 more sources
2023
Monitoring and predicting fault slip behaviors in subduction zones are essential for understanding earthquake cycles and assessing future earthquake potential. We developed a data assimilation (DA) method for fault slip monitoring and short-term prediction of slow slip events (SSEs), which was applied to the 2010 Bungo Channel SSE in southwest Japan ...
Masayuki Kano +4 more
openaire +1 more source
Monitoring and predicting fault slip behaviors in subduction zones are essential for understanding earthquake cycles and assessing future earthquake potential. We developed a data assimilation (DA) method for fault slip monitoring and short-term prediction of slow slip events (SSEs), which was applied to the 2010 Bungo Channel SSE in southwest Japan ...
Masayuki Kano +4 more
openaire +1 more source

