The Alaska Convergent Margin Backstop Splay Fault Zone, a Potential Large Tsunami Generator Between the Frontal Prism and Continental Framework
Author:
Affiliation:
1. U.S. Geological Survey Emeritus Moffett Field CA USA
2. U.S. Geological Survey Emeritus Denver Federal Center Denver CO USA
3. GEOMAR Helmholtz Centre for Ocean Research Kiel Germany
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GC008901
Reference76 articles.
1. Gravity anomalies, crustal structure, and seismicity at subduction zones: 2. Interrelationships between fore-arc structure and seismogenic behavior
2. Tsunamigenic structures in a creeping section of the Alaska subduction zone;Bécel A.;Nature Geoscience,2017
3. Rigidity variations with depth along interplate megathrust faults in subduction zones
4. Subduction zone megathrust earthquakes
5. Uplift and subsidence reveal a nonpersistent megathrust rupture boundary (Sitkinak Island, Alaska)
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