Results 151 to 160 of about 713 (187)
Coral geochemical response to uplift in the aftermath of the 2005 Nias-Simeulue earthquake. [PDF]
Sosdian SM +9 more
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Foreshock-induced slip transients set mainshock nucleation timing. [PDF]
Fryer B +3 more
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From foreshock to mainshock: transient sliding velocity sets nucleation time
Fryer B +3 more
europepmc +1 more source
Effects of slope instability on coseismic landslide susceptibility during earthquakes
openaire
Limits to coseismic landslides triggered by Cascadia Subduction Zone earthquakes
Landslides are a significant hazard and dominant feature throughout the landscape of the Pacific Northwest. However, the hazard and risk posed by coseismic landslides triggered by great Cascadia Subduction Zone (CSZ) earthquakes is highly uncertain due to a lack of local and global data.
William T Struble, Sean R Lahusen
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This research aims to explore detailed spatial distribution characteristics, identify key factors weight, and establish an accurate susceptibility regionalization model of coseismic landslides by the Mw 6.6 Iburi, Japan, earthquake sequence of 6 ...
Ming Chang +2 more
exaly +2 more sources
A numerical simulation of seismic signals of coseismic landslides
Engineering Geology, 2021Abstract When a coseismic landslide is triggered by an earthquake, seismic stations close to the location of the landslide will simultaneously record the seismic signals caused by the earthquake and landslide, causing confusion between the two signals.
Zheng-Yi Feng
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Coseismic landslides triggered by the 2022 Luding Ms6.8 earthquake, China
Landslides, 2023Lanxin Dai +2 more
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Hybrid Computational Intelligence Modeling of Coseismic Landslides’ Severity
2021Coseismic Landslides (COLA) are one of the most widespread and destructive hazards to result from earthquakes in mountainous environments. They are always associated with almost instantaneous slope collapse and spreading, posing significant hazards to human lives and lifeline facilities worldwide.
Anastasios Panagiotis Psathas +4 more
openaire +1 more source

