A thermochemical calculation of the pyroxene saturation surface in the system diopside-albite-anorthite

R. Hon, D. J. Henry, A. Navrotsky, D. F. Weill

Research output: Contribution to journalArticlepeer-review

21 Scopus citations

Abstract

The pyroxene saturation surface in the system diopside-albite-anorthite may be calculated to ±10°C from thermochemical data over most of its composition range. The thermochemical data used are the experimentally determined enthalpies of mixing of the ternary liquids and the enthalpy of fusion of diopside. These are combined with a mixing model for the configurational entropy in the melt and the activity of CaMgSi2O6 in the clinopyroxene, which is less than unity due to departures from CaMgSi2O6 stoichiometry. The 'two-lattice' melt model appears to work satisfactorily throughout the pyroxene primary phase field but probably needs modification at more anorthite-rich compositions.

Original languageEnglish (US)
Pages (from-to)157-161
Number of pages5
JournalGeochimica et Cosmochimica Acta
Volume45
Issue number2
DOIs
StatePublished - Feb 1981

ASJC Scopus subject areas

  • Geochemistry and Petrology

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