Equations of state of close-packed phases of iron and their implications for the Earth's core-Reference-Cited by-同舟云学术

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Equations of state of close-packed phases of iron and their implications for the Earth's core

Published:1979-01 Issue:1 Volume:18 Page:13-19
ISSN:0031-9201
Container-title:Physics of the Earth and Planetary Interiors
language:en
Short-container-title:Physics of the Earth and Planetary Interiors

Author:

Mulargia F.,Boschi E.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference26 articles.

1. Shock adiabats and zero isotherms of seven metals at high pressures;Al'tshuler;Sov. Phys. — JETP,1962

2. An Earth model based on free oscillation and body waves;Anderson;J. Geophys. Res.,1976

3. Shock compression of two iron silicon alloys to 2.7 megabars;Balchan;J. Geophys. Res.,1966

4. Elasticity and constitution of the Earth's interior;Birch;J. Geophys. Res.,1952

5. The Structure of the Elements;Donahue,1974

Cited by 11 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Volume variation of Gruneisen parameters offcc transition metals;Bulletin of Materials Science;2002-02

2. Thermal properties of iron at high pressures and temperatures;Physical Review B;1996-04-01

3. Phase transitions, Grüneisen parameter, and elasticity for shocked iron between 77 GPa and 400 GPa;Journal of Geophysical Research: Solid Earth;1986-06-10

4. Thermodynamics;The Physics of the Earth's Core;1986

5. A new equation of state for high compression;Physics of the Earth and Planetary Interiors;1982-10

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