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The source scaling of swarm-genic slow slip events
2020<p>Slow slip events (SSEs) are slow fault ruptures that do not excite detectable seismic waves although they are often accompanied by some forms of seismic strain release, e.g., clusters of low- and very-low frequency earthquakes, and/or episodic or continuous non-volcanic tremor (i.e.
Luigi Passarelli +3 more
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Fault-valve instability: A mechanism for slow slip events
Journal of Geophysical Research: Solid EarthAbstract Geophysical and geological studies provide evidence for cyclic changes in fault‐zone pore fluid pressure that synchronize with or at least modulate slip events. A hypothesized explanation is fault valving arising from temporal changes in fault zone permeability.
So Ozawa, Yuyun Yang, Eric M Dunham
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Episodic slow slip events and rate‐and‐state friction
Journal of Geophysical Research: Solid Earth, 2008There are several ways of generating episodic slow slip events in models of rate‐and‐state friction. Here I explore the possibility that they arise on velocity‐weakening faults whose length is “tuned” in some sense. Unlike spring‐block sliders, which have a unique critical stiffness for instability, elastically deformable faults have multiple length ...
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Slow slip events and seismic tremor at circum‐Pacific subduction zones
Reviews of Geophysics, 2007Susan Y Schwartz
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Fast and Slow Slip Events Emerge Due to Fault Geometrical Complexity
Geophysical Research Letters, 2018Pierre Romanet +2 more
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Multiple slow‐slip events during a foreshock sequence of the 2014 Iquique, Chile Mw 8.1 earthquake
Geophysical Research Letters, 2014Aitaro Kato, Shigeki Nakagawa
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Kilauea slow slip events: Identification, source inversions, and relation to seismicity
Journal of Geophysical Research, 2009E K Montgomery-Brown +2 more
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