Seismic Attenuation at the Equatorial Mid‐Atlantic Ridge Constrained by Local Rayleigh Wave Analysis From the PI‐LAB Experiment
Author:
Affiliation:
1. Ocean and Earth Science, University of Southampton Southampton UK
2. Department of Earth and Climate Science Indian Institute of Science Education and Research Tirupati Tirupati India
3. Deparment of Earth Sciences University of Oxford Oxford UK
Funder
Natural Environment Research Council
FP7 Ideas: European Research Council
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC010085
Reference111 articles.
1. Reconciling mantle attenuation-temperature relationships from seismology, petrology, and laboratory measurements
2. Sediment Characterization at the Equatorial Mid‐Atlantic Ridge From P ‐to‐ S Teleseismic Phase Conversions Recorded on the PI‐LAB Experiment
3. A thin mantle transition zone beneath the equatorial Mid-Atlantic Ridge
4. Lithosphere–asthenosphere boundary beneath the Sea of Japan from transdimensional inversion of S-receiver functions
5. Time-dependent models of U–Th–He and K–Ar evolution and the layering of mantle convection
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