Mutually consistent estimates of upper mantle composition from seismic velocity contrasts at 400 km depth-Reference-Cited by-同舟云学术

Mutually consistent estimates of upper mantle composition from seismic velocity contrasts at 400 km depth

Published:1993 Issue:1 Volume:141 Page:101-109
ISSN:0033-4553
Container-title:Pure and Applied Geophysics PAGEOPH
language:en
Short-container-title:PAGEOPH

Author:

Bina Craig R.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00876237.pdf

Reference49 articles.

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2. Akaogi, M., andAkimoto, S. (1977),Pyroxene-garnet Solid-solution Equilibria in the Systems Mg 4 Si 4 O 12?Mg 3 Al 2 Si 3 O 12 and Fe 4 Si 4 O 12?Fe 3 Al 2 Si 3 O 12 at High Pressures and Temperatures, Phys. Earth Planet. Inter.15, 90?106.

3. Akaogi, M., Navrotsky, A., Yagi, T., andAkimoto, S., Pyroxene-garnet transformation: Thermochemistry and elasticity of garnet solids solutions, and application to a pyrolite mantle. InHigh-pressure Research in Mineral Physics (eds. Manghnani, M. H., and Syono, Y.) (Terra Scientific, Tokyo 1987) pp. 251?260.

4. Akaogi, M., Ross, N. L., McMillan, P., andNavrotsky, A. (1984),The Mg 2 SiO 4 Polymorphs (Olivine, Modified Spinel, and Spinel) ? Thermodynamic Properties from Oxide Melt Solution Calorimetry, Phase Relations, and Models of Lattice Vibrations, Am. Mineral.69, 499?512.

5. Akimoto, S., andFujisawa, H. (1968),Olivine-spinel Solid Solution Equilibria in the System Mg 2 SiO 4?Fe 2 SiO 4, J. Geophys. Res.73, 1467?1479.

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