Results 11 to 20 of about 2,166,063 (293)
Origin of slow earthquake statistics in low-friction soft granular shear [PDF]
Nature CommunicationsSlow earthquakes differ from regular earthquakes in their slower moment release and size distribution dominated by smaller events. However, the physical origin of these slow earthquake statistics remains controversial.
Yuto Sasaki, Hiroaki Katsuragi
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Geochemistry, Geophysics, Geosystems, 2020 The month‐to‐year‐long deformation of the Earth's crust where active subduction zones terminate is poorly explored. Here we report on a multidisciplinary data set that captures the synergy of slow‐slip events, earthquake swarms and fault interactions ...
Jonathan Bedford +2 more
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Slow earthquake scaling reconsidered as a boundary between distinct modes of rupture propagation. [PDF]
Proc Natl Acad Sci U S A, 2023 Significance Slow earthquakes were discovered ~ 20 y ago and have been studied extensively. In 2007, we proposed a scaling law for slow earthquakes.
Ide S, Beroza GC.
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Slow earthquake in Afghanistan detected by InSAR [PDF]
Geophysical Research Letters, 2008 The Chaman fault system forms a prominent ∼900‐km‐long left‐lateral transform plate boundary between the Indian and Eurasian plates in Afghanistan and Pakistan. Here we show satellite radar interferometry data that revealed an afterslip (or slow earthquake) signal following an earthquake of magnitude 5.0.
Masato Furuya
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Relationship of preseismic, coseismic, and postseismic fault ruptures of two large interplate aftershocks of the 2011 Tohoku earthquake with slow-earthquake activity. [PDF]
Sci Rep, 2020 To improve our understanding of the interactions between regular and slow earthquakes along the Japan Trench, we investigated the spatial relationship of slow-earthquake activity with the preseismic, coseismic, and postseismic fault ruptures of ...
Kubo H, Nishikawa T.
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Geophysical Research Letters, 2023 Earthquake‐triggered slow‐moving landslides are not well studied mainly due to a lack of high‐resolution in‐situ geodetic observations both in time and space.
Yunmeng Cao +3 more
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Geochemistry, Geophysics, Geosystems, 2020 Field studies have led to several interpretations on the mechanics behind slow earthquake phenomena downdip of the seismogenic zone. To date, field studies have not examined the shallow subduction interface which may also host slow earthquake phenomena ...
Noah John Phillips +3 more
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Remote Sensing, 2023 Strong earthquakes can not only trigger many landslides in a short period of time but can also change the stability of slopes in the earthquake area, causing them to be active for a long time after the earthquake. Research on the variation of slow-motion
Rong Gui, Jun Hu, Gui Rong
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Journal of Geophysical Research: Solid Earth, 2021 Earthquake swarms, which are anomalous increases in the seismicity rate without a distinguishable mainshock, often accompany transient aseismic processes, such as fluid migration and episodic aseismic slip along faults. Investigations of earthquake swarm
Tomoaki Nishikawa +2 more
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Slow slip modulates low-frequency seismicity on the Parkfield segment of the San Andreas Fault [PDF]
Nature CommunicationsUnderstanding how slow slip events (SSEs) influence fault behavior is essential for characterizing the fault slip spectrum and its role in earthquake generation.
Zahra Zali +3 more
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