Assessing Margin‐Wide Rupture Behaviors Along the Cascadia Megathrust With 3‐D Dynamic Rupture Simulations-Reference-Cited by-同舟云学术

Assessing Margin‐Wide Rupture Behaviors Along the Cascadia Megathrust With 3‐D Dynamic Rupture Simulations

Published:2021-07 Issue:7 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J Geophys Res Solid Earth

Author:

Ramos Marlon D.¹^ORCID,Huang Yihe¹^ORCID,Ulrich Thomas²^ORCID,Li Duo²^ORCID,Gabriel Alice‐Agnes²³^ORCID,Thomas Amanda M.⁴^ORCID

Affiliation:

1. Department of Earth and Environmental Sciences University of Michigan Ann Arbor MI USA

2. Department of Earth and Environmental Sciences Ludwig‐Maximilians‐Universität München Munchen Germany

3. Institute of Geophysics and Planetary Physics Scripps Institution of Oceanography University of California San Diego La Jolla CA USA

4. Department of Earth Sciences University of Oregon Eugene OR USA

Funder

National Science Foundation

FP7 Ideas: European Research Council

Bayerisch-Kalifornischen Hochschulzentrum

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB022005

Reference101 articles.

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2. Deep‐sea turbidites as guides to Holocene earthquake history at the Cascadia Subduction Zone—Alternative views for a seismic‐hazard workshop;Atwater B. F.;US Geological Survey Open‐File Report,2012

3. Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing

4. Permanent deformation caused by subduction earthquakes in northern Chile

5. A Long‐Term View of Episodic Tremor and Slip in Cascadia

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