Mantle transition zone structure and upper mantle S velocity variations beneath Ethiopia: Evidence for a broad, deep-seated thermal anomaly-Reference-Cited by-同舟云学术

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Mantle transition zone structure and upper mantle S velocity variations beneath Ethiopia: Evidence for a broad, deep-seated thermal anomaly

Published:2006-11 Issue:11 Volume:7 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Benoit Margaret H.,Nyblade Andrew A.¹,Owens Thomas J.²,Stuart Graham³

Affiliation:

1. Department of Geosciences; Penn State University; University Park; Pennsylvania; 16801; USA

2. Department of Geological Sciences; University of South Carolina; Columbia; South Carolina; 29201; USA

3. School of Earth and Environment; University of Leeds; Leeds; LS2 9JT; UK

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference57 articles.

1. Origin and timing of Ethiopian ignimbrites;Ayalew;Geophys. J.,2002

2. A brief Oligocene period of flood volcanism in Yemen;Baker;Earth Planet. Sci. Lett.,1996

3. Upper mantle seismic structure in a region of incipient continental breakup: Northern Ethiopian rift;Bastow;Geophys. J. Int.,2005

4. Upper mantle P wave speed variations beneath Ethiopia and the origin of the Afar Hotspot;Benoit;Geology,2006

5. Phase transition Clapeyron slopes and transition zone seismic discontinuity topography;Bina;J. Geophys. Res.,1994

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