Development of anisotropic contiguity in deforming partially molten aggregates: 2. Implications for the lithosphere‐asthenosphere boundary
Author:
Affiliation:
1. Department of Earth Sciences Royal Holloway University of London Egham UK
2. Applied Math, Statistics, and Scientific Computation University of Maryland College Park Maryland USA
Funder
National Science Foundation
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/2014JB011454
Reference33 articles.
1. Changes in Seismic Anisotropy Shed Light on the Nature of the Gutenberg Discontinuity
2. Influence of deformation on melt topology in peridotites
3. Development of anisotropic contiguity in deforming partially molten aggregates: 1. Theory and fast multipole boundary elements method
4. Geophysical evidence from the MELT area for compositional controls on oceanic plates
5. The Lithosphere-Asthenosphere Boundary
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