Constraints on asthenospheric flow from the depths of oceanic spreading centers: The East Pacific Rise and the Australian-Antarctic Discordance-Reference-Cited by-同舟云学术

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Constraints on asthenospheric flow from the depths of oceanic spreading centers: The East Pacific Rise and the Australian-Antarctic Discordance

Published:2009-09 Issue:9 Volume:10 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Buck W. Roger¹,Small Christopher¹,Ryan William B. F.¹

Affiliation:

1. Lamont-Doherty Earth Observatory; Earth Institute at Columbia University; Palisades; New York; 10964; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference89 articles.

1. Channeling of plume flow beneath mid-ocean ridges;Albers;Earth Planet. Sci. Lett.,2001

2. Geologic evidence for the plate driving mechanism: The continental undertow hypothesis and the Australian-Antarctic Discordance;Alvarez;Tectonics,1990

3. Variations in upper crustal structure due to variable mantle temperature along the Southeast Indian Ridge;Baran;Geochem. Geophys. Geosyst.,2005

4. Comparison of azimuthal seismic anisotropy from surface waves and finite strain from global mantle-circulation models;Becker;Geophys. J. Int.,2003

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