An anisotropic equation of state for solid solutions, with application to plagioclase

R. Myhill*

*Corresponding author for this work

Research output: Contribution to journalArticle (Academic Journal)peer-review

Abstract

This paper presents a framework for building anisotropic equations of state for solid solutions. The framework satisfies the connections between elastic and thermodynamic properties required by Maxwell's relations. It builds on a recent anisotropic equation of state for pure phases under small deviatoric stresses, adding a dependence on a vector, whose components contain the molar amounts of independent end-members in the solid solution. These end-members may have distinct chemical compositions, site species occupancies or electronic spin states. The high albite-anorthite (C) plagioclase solid solution is used to illustrate the formulation.

Original languageEnglish
Pages (from-to)1900-1909
Number of pages10
JournalGeophysical Journal International
Volume239
Issue number3
Early online date14 Oct 2024
DOIs
Publication statusPublished - 1 Dec 2024

Bibliographical note

Publisher Copyright:
© 2024 The Author(s). Published by Oxford University Press on behalf of The Royal Astronomical Society.

Keywords

  • Elasticity and anelasticity
  • Equations of state
  • Seismic anisotropy

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