Results 11 to 20 of about 882,743 (301)
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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A review on slow earthquakes in the Japan Trench
Progress in Earth and Planetary Science, 2023 Slow earthquakes are episodic slow fault slips. They form a fundamental component of interplate deformation processes, along with fast, regular earthquakes.
Tomoaki Nishikawa +2 more
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Slow earthquake scaling reconsidered as a boundary between distinct modes of rupture propagation [PDF]
Proceedings of the National Academy of Sciences of the United States of America, 2023 Gregory C. Beroza, Satoshi Ide
exaly +2 more sources
Slow Earthquakes in the Microseism Frequency Band (0.1–1.0 Hz) off Kii Peninsula, Japan
Geophysical Research Letters, 2018 It is difficult to detect the signal of slow deformation in the 0.1–1.0 Hz frequency band between tectonic tremors and very low frequency events, where microseism noise is dominant.
Lisa Kaneko, Masaru Nakano, Satoshi Ide
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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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Physics of the Earth and Planetary Interiors, 1979 Anomalous earthquakes such as creep events, tsunami earthquakes and silent earthquakes have been reported in the recent literature. In this paper we discuss an anomalous “slow earthquake” that occurred on June 6, 1960 in southern Chile.
Stewart, Gordon S., Kanamori, Hiroo
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The predictable chaos of slow earthquakes [PDF]
Science Advances, 2020 Slow earthquakes result from deterministic chaos and show predictability horizon time of the order of days to weeks.
Gualandi, A. +3 more
openaire +3 more sources
Frontiers in Earth Science, 2022 The southernmost Ryukyu subduction zone may have a geodetically inferred Mw 7.5 to 8.7 megathrust earthquake in a shallow locked region, the Ryukyu fault.
Sean Kuanhsiang Chen +4 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
Caihong He, Qian Sun, Jun Hu, Rong Gui
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Slow slip events following the afterslip of the 2002 Mw 7.1 Hualien offshore earthquake, Taiwan
Earth, Planets and Space, 2022 Geodetic evidence for slow slip recurrence changed by stress perturbations was rare, especially from afterslip following a nearby large earthquake. The first observed slow slip events in the southernmost Ryukyu subduction had occurred in 2005, 2009, and ...
Sean Kuanhsiang Chen +2 more
doaj +1 more source