Abstract
The methods described so far have been used in investigations of the earth’s interior [1–7]. The earth is a natural high-pressure laboratory and provides a convenient object for the application of the methods used in high-pressure physics, which yield very illuminating information about the earth’s interior. Such applications to the physics of the earth were begun in 1952 by Magnitskii [8–10] and Birch [11].
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Zharkov, V.N., Kalinin, V.A. (1971). Applications of Equations of State to the Physics of the Earth’s Interior. In: Equations of State for Solids at High Pressures and Temperatures. Springer, Boston, MA. https://doi.org/10.1007/978-1-4757-1517-0_7
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DOI: https://doi.org/10.1007/978-1-4757-1517-0_7
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