Lithospheric instability and the source of the Cameroon Volcanic Line: Evidence from Rayleigh wave phase velocity tomography-Reference-Cited by-同舟云学术

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Lithospheric instability and the source of the Cameroon Volcanic Line: Evidence from Rayleigh wave phase velocity tomography

Published:2015-03 Issue:3 Volume:120 Page:1708-1727
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Adams Aubreya N.¹,Wiens Douglas A.¹,Nyblade Andrew A.²,Euler Garrett G.³,Shore Patrick J.¹,Tibi Rigobert⁴

Affiliation:

1. Department of Earth and Planetary Sciences; Washington University in St. Louis; Saint Louis Missouri USA

2. Department of Geosciences; Penn State University; University Park Pennsylvania USA

3. Los Alamos National Laboratory; New Mexico USA

4. Global Geophysical Services, Inc.; Denver, Colorado USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference83 articles.

1. Shear wave velocity structure of the southern African upper mantle with implications for the uplift of southern Africa;Adams;Geophys. J. Int.,2011

2. Upper mantle shear wave velocity structure beneath the East African plateau: Evidence for a deep, plateau wide low velocity anomaly;Adams;Geophys. J. Int.,2012

3. Cosmogenic helium and neon in mantle xenoliths from the Cameroon Volcanic Line (West Africa): Preliminary observations;Aka;J. Afr. Earth Sci.,2009

4. The current limits of resolution for surface wave tomography in North America;Bassin;Eos Trans. AGU,2000

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