Upper Mantle Anisotropic Shear Velocity Structure at the Equatorial Mid‐Atlantic Ridge Constrained by Rayleigh Wave Group Velocity Analysis From the PI‐LAB Experiment-Reference-Cited by-同舟云学术

Upper Mantle Anisotropic Shear Velocity Structure at the Equatorial Mid‐Atlantic Ridge Constrained by Rayleigh Wave Group Velocity Analysis From the PI‐LAB Experiment

Published:2021-03 Issue:3 Volume:22 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Saikia Utpal¹^ORCID,Rychert Catherine¹^ORCID,Harmon Nicholas¹^ORCID,Kendall J. M.²

Affiliation:

1. Ocean and Earth Science University of Southampton Southampton University UK

2. School of Earth Sciences University of Oxford Oxford UK

Funder

National Research Council

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GC009495

Reference104 articles.

1. Sediment Characterization at the Equatorial Mid‐Atlantic Ridge From P ‐to‐ S Teleseismic Phase Conversions Recorded on the PI‐LAB Experiment

2. Partial melting and the low-velocity zone

3. Shear wave splitting and crustal anisotropy at the Mid-Atlantic Ridge, 35°N

4. Implications of grain size evolution on the seismic structure of the oceanic upper mantle

5. Ridge asymmetry and deep aqueous alteration at the trench observed from Rayleigh wave tomography of the Juan de Fuca plate

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