Results 21 to 30 of about 7,254 (288)
Frictional Mechanics of Slow Earthquakes [PDF]
Journal of Geophysical Research: Solid Earth, 2018 AbstractTectonic faults slip in a wide range of modes that span from slow slip events to dynamic rupture. A growing body of observations document this spectrum of failure modes in many geologic settings. However, the physical mechanisms that dictate slow slip are not understood.
J. R. Leeman, C. Marone, D. M. Saffer
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Recent Crustal Deformation in West-Central South America [PDF]
, 2003 I use interferometric synthetic aperture radar (InSAR) to create maps of crustal deformation along the coast and within the volcanic arc of central South America. I image deformation associated with six subduction zone earthquakes, four volcanic centers,
Pritchard, Matthew Earl
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Bridging the gap between low-frequency and very-low-frequency earthquakes
Earth, Planets and Space, 2020 Slow earthquakes that are observed in the > 1 Hz frequency band are called tectonic tremor or low-frequency earthquakes (LFEs) and those in the 0.01–0.10 Hz band are called very-low-frequency earthquakes (VLFEs).
Koki Masuda +3 more
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Nature Communications, 2022 Laboratory earthquake experiments reproduce delayed earthquake triggering, similar to aftershocks, as a result of propagating slow slip fronts. The speed of the fronts can be highly sensitive to fault stress levels left behind by previous earthquakes.
Sara Beth L. Cebry +5 more
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Characteristics of Slow Slip Event in March 2020 Revealed From Borehole and DONET Observatories
Frontiers in Earth Science, 2021 We have detected an event of pore pressure change (hereafter, we refer it to “pore pressure event”) from borehole stations in real time in March 2020, owing to the network developed by connecting three borehole stations to the Dense Oceanfloor Network ...
Keisuke Ariyoshi +13 more
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Static Source Properties of Slow and Fast Earthquakes [PDF]
Journal of Geophysical Research: Solid Earth, 2020 AbstractThe source characteristics of slow and fast earthquakes provide a window into the mechanical properties of faults. In particular, the average stress drop controls the evolution of friction, fault slip, and event magnitude. However, this important source property is typically inferred from the analysis of seismic waves and is subject to many ...
Priyamvada Nanjundiah +2 more
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Geophysical Research Letters, 2023 Off Cape Muroto area, along the Nankai Trough in southwest Japan, is a typical area with adjacent occurrences of slow and megathrust earthquakes. High‐resolution monitoring of slow earthquakes is necessary to understand tectonic conditions.
Satoru Baba +7 more
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Haiti - The Slow Road to Reconstruction: Two years after the earthquake [PDF]
, 2012 After two years Haitians continue to grapple with the effects of the devastating earthquake that killed more than 200,000 people and rendered more than one million homeless.
Cohen, Marc J.
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Long-range, critical-point dynamics in oil field flow rate data [PDF]
, 2006 Earthquake triggering data exhibit long-range spatio-temporal correlations of the power-law form C(l) ∼ l−α and anomalously-slow temporal diffusion of the mean triggering distance of the form: 〈l〉 ∼ tH, with H < 0.5.
Papasouliotis, O. +6 more
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Original data for the manuscript "The role of preseismic slow slip in earthquake incubation".
, 2023 Original data for the manuscript "The role of preseismic slow slip in earthquake incubation".
Peng Dong (11977931)
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