Development of anisotropic structure in the Earth's lower mantle by solid-state convection
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/416310a.pdf
Reference24 articles.
1. Lay, T., Williams, Q. & Garnero, E. J. The core–mantle boundary layer and deep Earth dynamics. Nature 392, 461–468 (1998).
2. Lay, T., Williams, Q., Garnero, E. J., Kellogg, L. & Wysession, M. E. in The Core-Mantle Boundary (eds Gurnis, M., Wysession, M. E., Knittle, E. & Buffett, B. A.) 299–318 (Geodynamics Series Vol. 28, Am. Geophys. Union, Washington DC, 1998).
3. Kendall, J. M. in Earth's Deep Interior: Mineral Physics and Tomography from the Atomic to the Global Scale (eds Karato, S., Forte, A. M., Liebermann, R. C., Masters, G. & Stixrude, L.) 133–159 (Geophysics Monograph 117, Am. Geophys. Union, Washington DC, 2000).
4. Ritsema, J. Evidence for shear velocity anisotropy in the lowermost mantle beneath the Indian Ocean. Geophys. Res. Lett. 27, 1041–1044 (2000).
5. Kendall, J. M. & Silver, P. G. Constraints from seismic anisotropy on the nature of the lowermost mantle. Nature 381, 409–412 (1996).
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