Mapping the Lithosphere and Asthenosphere Beneath Alaska With Sp Converted Waves
Author:
Affiliation:
1. Department of Earth, Environmental and Planetary Sciences Brown University Providence RI USA
2. Jackson School of Geosciences University of Texas at Austin Austin TX USA
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GC010517
Reference124 articles.
1. Reconciling mantle attenuation-temperature relationships from seismology, petrology, and laboratory measurements
2. North American lithospheric discontinuity structure imaged byPsandSpreceiver functions
3. Ten kilometer vertical Moho offset and shallow velocity contrast along the Denali fault zone from double-difference tomography, receiver functions, and fault zone head waves
4. Dike swarms on Seward Peninsula, Alaska, and their implications for the kinematics of Cretaceous extension in the Bering Strait region
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1. Along‐Strike Variations of Alaska Subduction Zone Structure and Hydration Determined From Amphibious Seismic Data;Journal of Geophysical Research: Solid Earth;2024-03
2. Anisotropic structure of the normally-dipping and flat slab segments of the Alaska subduction zone: Insights from receiver function analysis;Tectonophysics;2023-12
3. Equilibration depth and temperature of Neogene alkaline lavas in the Cordillera of Alaska and Canada as a constraint on the lithosphere–asthenosphere boundary;Canadian Journal of Earth Sciences;2023-08-01
4. The Upper‐Mantle Structure Beneath Alaska Imaged by Teleseismic S‐Wave Reverberations;Journal of Geophysical Research: Solid Earth;2023-06
5. Variations in Lithospheric Thickness Across the Denali Fault and in Northern Alaska;Geophysical Research Letters;2022-12-22
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