A modeling of the structure and compressibility of quartz with a molecular potential and its transferability to cristobalite and coesite-Reference-Cited by-同舟云学术

A modeling of the structure and compressibility of quartz with a molecular potential and its transferability to cristobalite and coesite

Published:1993-07 Issue:2 Volume:20 Page:123-135
ISSN:0342-1791
Container-title:Physics and Chemistry of Minerals
language:en
Short-container-title:Phys Chem Minerals

Author:

Boisen M. B.,Gibbs G. V.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,General Materials Science

Link

http://link.springer.com/content/pdf/10.1007/BF00207206.pdf

Reference40 articles.

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2. Bassett WA, Barnett JD (1970) Isothermal compression of stishovite and coesite up to 85 kilobars at room temperature by X-ray diffraction. Phys Earth Planet Inter 3:54–60

3. Birch F (1938) The effect of pressure upon the elastic parameters of isotropic solids, according to Murnaghan's theory of finite strain. J Appl Phys 9:279–288

4. Birch F (1952) Elasticity and constitution of the earth's interior. J Geophys Res 57:227–286

5. Boisen MB Jr, Gibbs GV, Downs RT, D'Arco P (1990) The dependence of the SiO bond length on structural parameters in coesite, the silica polymorphs and the clathrasils. Am Mineral 75:748–754

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