Evolution of the Oceanic Lithosphere in the Equatorial Atlantic From Rayleigh Wave Tomography, Evidence for Small‐Scale Convection From the PI‐LAB Experiment

Evolution of the Oceanic Lithosphere in the Equatorial Atlantic From Rayleigh Wave Tomography, Evidence for Small‐Scale Convection From the PI‐LAB Experiment

Abstract The oceanic lithosphere is a primary component of the plate tectonic system, yet its evolution and its asthenospheric interaction have rarely been quantified by in situ imaging at slow spreading systems. We use Rayleigh wave tomography from noise and teleseismic surface waves to image the s...

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Bibliographic Details
Main Authors: Nicholas Harmon, Catherine A. Rychert, J. Michael Kendall, Matthew Agius, Petros Bogiatzis, Saikiran Tharimena
Format: Article
Language:English
Published: Wiley 2020-09-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
surface wave tomography
shear velocity
oceanic lithosphere
asthenosphere
Atlantic Ocean
PI‐LAB
Online Access:https://doi.org/10.1029/2020GC009174

Internet

https://doi.org/10.1029/2020GC009174

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