Detecting lithospheric discontinuities beneath the Mississippi Embayment using S-wave receiver functions
Author:
Affiliation:
1. Center for Earthquake Research and Information, University of Memphis, Memphis, TN 38152, USA
2. Department of Geological Sciences, University of Florida, Gainesville, FL 32611, USA
Abstract
Funder
University of Memphis
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggab367/40331878/ggab367.pdf
Reference67 articles.
1. North American lithospheric discontinuity structure imaged by PS and SP receiver functions;Abt;J. geophys. Res.,2010
2. On the nonuniqueness of receiver function inversions;Ammon;J. geophys. Res.,1990
3. ObsPy: A Python toolbox for seismology;Beyreuther;Seismol. Res. Lett.,2010
4. Relationship between observed upper mantle structures and recent tectonic activity across the Southeastern United States;Biryol;J. geophys. Res.,2016
5. Mantle stratigraphy and evolution of the Slave province;Bostock;J. geophys. Res.,1998
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1. High P‐T Sound Velocities of Amphiboles: Implications for Low‐Velocity Anomalies in Metasomatized Upper Mantle;Geophysical Research Letters;2024-02-28
2. Roles of Continental Mid‐Lithosphere Discontinuity in the Craton Instability Under Variable Tectonic Regimes;Journal of Geophysical Research: Solid Earth;2024-01
3. Continental Mid‐Lithosphere Discontinuity: A Water Collector During Craton Evolution;Geophysical Research Letters;2022-12
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