Tsunamigenic Splay Faults Imply a Long‐Term Asperity in Southern Prince William Sound, Alaska
Author:
Affiliation:
1. Department of Geosciences Boise State University Boise ID USA
2. Pacific Coastal and Marine Science Center U.S. Geological Survey Santa Cruz CA USA
3. U.S. Geological Survey Anchorage AK USA
Funder
U.S. Geological Survey
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL081528
Reference47 articles.
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2. Balster‐Gee A. F. Brothers D. S. Finlayson D. P. Liberty L. M. Dartnell P. Hatcher G. A. Haeussler P. J. Byerly M.(2019).Bathymetry acoustic backscatter and minisparker seismic‐reflection datasets collected southwest of Montague Island and southwest of Chenega Island Alaska during field activity 2014‐622‐FA. U.S. Geological Survey Data Release.https://doi.org/10.5066/P9K1YQ35
3. Tsunamigenic structures in a creeping section of the Alaska subduction zone
4. Mapping the megathrust beneath the northern Gulf of Alaska using wide-angle seismic data
5. A submarine landslide source for the devastating 1964 Chenega tsunami, southern Alaska
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