Results 11 to 20 of about 910,751 (157)
Frontiers in Earth Science, 2021 In our recent study, we detected the pore pressure change due to the slow slip event (SSE) in March 2020 at the two borehole stations (C0002 and C0010), where the other borehole (C0006) close to the Nankai Trough seems not because of instrumental drift ...
Keisuke Ariyoshi +14 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)
core +1 more source
Recovery of the recurrence interval of Boso slow slip events in Japan
Earth, Planets and Space, 2019 We present the spatiotemporal evolution of the Boso slow slip event with a moment of 20 × 1018 N m that occurred in June 2018; such events, which have a duration of 1–2 weeks, have repeatedly occurred off the Boso peninsula, east Japan.
Shinzaburo Ozawa +2 more
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Contribution of Turkish Scholars to Earthquake Literature: The Impact of the Marmara Earthquake [PDF]
, 2010 This paper addresses the question of whether the Marmara Earthquake of August 17, 1999, has had an impact on the contribution of Turkish scholars to the earthquake literature.
TAŞKIN, ZEHRA +2 more
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Earthquake Source Characterization Using 3D Numerical Modeling [PDF]
, 2007 To understand the physics of earthquakes, it is important to know what happens during individual events. Dissembling the information about the source process from the recorded seismograms is a difficult and non-unique process, as there are severe trade ...
Hjörleifsdóttir, Vala
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Earthquake source parameters of the 2009 Mw 7.8 Fiordland (New Zealand) earthquake from L-band InSAR observations [PDF]
, 2011 The 2009 MW7.8 Fiordland (New Zealand) earthquake is the largest to have occurred in New Zealand since the 1931 Mw 7.8 Hawke’s Bay earthquake, 1 000 km to the northwest.
Qu, W. +7 more
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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
doaj +1 more source
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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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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Post-earthquake assessment of moderately damaged reinforced concrete plastic hinges
, 2020 Modern reinforced concrete buildings are often designed to dissipate energy during strong earthquakes by permitting the controlled formation of plastic hinges. Plastic hinges require assessment of residual capacity in post-earthquake situations. However,
Marder, K +3 more
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