Results 1 to 10 of about 5,667 (223)

Cascadia Subduction Zone Residents’ Tsunami Evacuation Expectations

open access: yesGeosciences, 2022
The U.S. Pacific Northwest coast must be prepared to evacuate immediately after a Cascadia Subduction Zone earthquake. This requires coastal residents to understand the tsunami threat, have accurate expectations about warning sources, engage in preimpact
Michael K. Lindell   +2 more
doaj   +2 more sources

Anisotropic tomography of the Cascadia subduction zone

open access: yesPhysics of the Earth and Planetary Interiors, 2021
Abstract The first P-wave tomography of 3-D azimuthal and radial anisotropy of the Cascadia subduction zone is determined by inverting local and teleseismic arrival-time data. Fast-velocity directions (FVDs) of azimuthal anisotropy in the crust are generally trench-parallel, reflecting N-S compression along the Cascadia margin. Radial anisotropy (RAN)
Dapeng Zhao, Yuanyuan Hua
exaly   +2 more sources

A new chronology for tsunami deposits prior to the 1700 CE Cascadia earthquake from Vancouver Island, Canada [PDF]

open access: yesScientific Reports, 2022
Coastal deposits at Tofino, Ucluelet, and Port Alberni in Vancouver Island along the Cascadia subduction zone were re-examined to improve the earthquake history of the southwest coast of Canada.
Koichiro Tanigawa   +6 more
doaj   +2 more sources

Cascadia low frequency earthquakes at the base of an overpressured subduction shear zone [PDF]

open access: yesNature Communications, 2020
Regions of the subducting oceanic crust are often considered to be overpressured, owing to fluid trapped beneath an impermeable seal along the overlying inter-plate boundary.
Andrew J. Calvert   +3 more
doaj   +3 more sources

Seismic evidence for melt-rich lithosphere-asthenosphere boundary beneath young slab at Cascadia [PDF]

open access: yesNature Communications
The Lithosphere-Asthenosphere Boundary (LAB) beneath oceanic plates is generally imaged as a sharp seismic velocity reduction, suggesting the presence of partial melts.
Xin Wang   +5 more
doaj   +2 more sources

The Effect of Fore‐Arc Deformation on Shallow Earthquake Rupture Behavior in the Cascadia Subduction Zone

open access: yesGeophysical Research Letters, 2021
Within the fore‐arc of the Cascadia Subduction Zone, there are significant along‐strike differences in the orientation of splay faults, sediment consolidation, and fault roughness.
Khurram S. Aslam   +2 more
doaj   +2 more sources

Tectonic evolution of the Nootka fault zone and deformation of the shallow subducted Explorer plate in northern Cascadia as revealed by earthquake distributions and seismic tomography [PDF]

open access: yesScientific Reports, 2023
At the northern Cascadia subduction zone, the subducting Explorer and Juan de Fuca plates interact across a transform deformation zone, known as the Nootka fault zone (NFZ).
Jesse Hutchinson   +7 more
doaj   +2 more sources

Role of plate convergence rate in shaping earthquake recurrence in subduction zones [PDF]

open access: yesScientific Reports
Understanding the complex interplay of subduction zone processes is key to unravelling the timing and distribution of great earthquake cycles within the framework of the plate tectonics paradigm.
Sayak Ray   +4 more
doaj   +2 more sources

Filling the Gap in Cascadia: The Emergence of Low‐Amplitude Long‐Term Slow Slip

open access: yesGeochemistry, Geophysics, Geosystems, 2021
Long‐term slow slip events have been observed at several subduction zones around the globe, where they play an integral part in strain release along megathrust faults.
Carolyn P. Nuyen, David A. Schmidt
doaj   +1 more source

Statistical characterization of full-margin rupture recurrence for Cascadia subduction zone using event time resampling and Gaussian mixture model

open access: yesGeoscience Letters, 2023
Earthquake occurrence modeling of large subduction events involves significant uncertainty, stemming from the scarcity of geological data and inaccuracy of dating techniques.
Katsuichiro Goda
doaj   +1 more source

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