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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
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A Flying Start, Then a Slow Slip
Science, 2005The human tragedy caused by the Sumatra-Andaman earthquake (moment magnitude 9.3) on 26 December 2004 and its companion Nias earthquake (moment magnitude 8.7) on 28 March 2005 is difficult to comprehend. These earthquakes, the largest in 40 years, have also left seismologists searching for the words and tools to describe the enormity of the geological ...
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Science, 2010
Geology The largest earthquakes occur at subduction zones, which accommodate the convergence of two tectonic plates. Thanks to dense GPS and seismic networks along these zones, we have a more detailed, and now complicated, view of how this convergence occurs: Many subduction zones exhibit a phenomenon termed “slow slip.” Gomberg et al.
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Geology The largest earthquakes occur at subduction zones, which accommodate the convergence of two tectonic plates. Thanks to dense GPS and seismic networks along these zones, we have a more detailed, and now complicated, view of how this convergence occurs: Many subduction zones exhibit a phenomenon termed “slow slip.” Gomberg et al.
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Effects of material property variations on slip estimates for subduction interface slow‐slip events
We investigate the influence of elastic heterogeneity on geodetic inversions of slow-slip events by inverting for slip distributions of four events along the Hikurangi Margin, New Zealand.
Charles A Williams, Laura M Wallace
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Slip-plane and slip-cylinder theorems for slow viscous flow
Acta Mechanica, 1977Theorems for the slow two-dimensional flow of viscous fluids about slip-planes and slip-cylinders are proven. Examples of the use of the theorems are given.
Atanackovic, T. M., Leigh, D. C.
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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
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Science, 2016
Monitoring changes in the seafloor might be used for earthquake and tsunami ...
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Monitoring changes in the seafloor might be used for earthquake and tsunami ...
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Slow Crack Propagation and Slip Correlations
Pure and Applied Geophysics, 2003The propagation of an interfacial crack through a weak plane of a transparent Plexiglas block is studied experimentally. The toughness is controlled artificially by a sand blasting procedure, and fluctuates locally in space like uncorrelated random noise. The block is fractured in mode I at low speed (10’ - 10-4m/s).
Schmittbuhl, J. +4 more
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Slow slip: A new kind of earthquake
Physics Today, 2012Sandwiched between the shallow region of sudden, infrequent earthquakes and the deeper home to continuous viscous motion lies an intermediate realm of intermittent sliding and rumbling. Discovered in recent years, it still harbors many secrets.
John E. Vidale, Heidi Houston
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Slow Earthquakes, Preseismic Velocity Changes, and the Origin of Slow Frictional Stick-Slip
Science, 2013Slow Stick-Slip While the character of slow earthquakes has been approximated for some time, precise slip histories and the underlying mechanisms have remained elusive. Kaproth and Marone (p. 1229 ; published online 15 August) have made laboratory observations of repetitive, slow ...
Bryan M, Kaproth, C, Marone
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