The Elastic Anisotropy Change Near the 410‐km Discontinuity: Predictions From Single‐Crystal Elasticity Measurements of Olivine and Wadsleyite
Author:
Affiliation:
1. Institute of Meteoritics University of New Mexico Albuquerque NM USA
2. Department of Earth and Planetary Sciences University of New Mexico Albuquerque NM USA
3. Department of Geology University of Illinois Urbana‐Champaign IL USA
Funder
Division of Earth Sciences
University of New Mexico
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/10.1002/2017JB015339
Reference55 articles.
1. The elastic constants of San Carlos olivine to 17 GPa
2. Elasticity of Minerals, Glasses, and Melts
3. Composition of the upper mantle: Geophysical tests of two petrological models
4. Elasticity of a majorite-pyrope solid solution
5. Thermodynamic parameters in the Earth as determined from seismic profiles
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