Body Wave Speed Structure of Eastern North America

Abstract The eastern, passive margin of the North American continent is more heterogeneous than originally envisioned. Imaged by teleseismic body wave arrivals, both compressional Vp and shear Vsh, the lithospheric mantle of the stable, eastern North America contains rapid and large wave speed varia...

Full description

Bibliographic Details
Main Author: Brian Savage
Format: Article
Language:English
Published: Wiley 2021-01-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1029/2020GC009002