Evidence supporting the approximation γρ = const for the Grüneisen parameter of the Earth's lower mantle-Reference-Cited by-同舟云学术

Evidence supporting the approximation γρ = const for the Grüneisen parameter of the Earth's lower mantle

Published:1979-07-10 Issue:B7 Volume:84 Page:3537-3542
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res.

Author:

Anderson Orson L.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://www.agu.org/journals/jb/v084/iB07/JB084iB07p03537/JB084iB07p03537.pdf

Reference24 articles.

1. Equation for thermal expansivity in planetary interiors;Anderson;J. Geophys. Res.,1967

2. The high temperature acoustic Grüneisen parameter of the earth;Anderson;Phys. Earth Planet. Interiors,1979

3. The determination of the volume dependence of the Grüneisen parameter ϒ;Anderson;J. Geophys. Res.,1974

4. An experimentalist's equation of state: Avoiding the Grüneisen parameter quandry (abstract);Anderson;Eos Trans. AGU,1978

5. Some elastic constant data on minerals relevant to geophysics;Anderson;Rev. Geophys.,1968

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