The energetics of natural garnet solid solution - I. Mixing of the aluminosilicate end-members

Jibamitra Ganguly, George C. Kennedy

Research output: Contribution to journalArticle

89 Citations (Scopus)

Abstract

Approximate mixing properties of the end-member components of the quarternary garnet solid solution, (Fe,Mg,Ca,Mn)3Al2Si3O12, have been derived through theoretical analysis of observational data, combined with certain experimental results and crystal chemical considerations. The results suggest that the mixing of pyrope with grossularite, spessartite, and almandine would involve significant positive excess free energies of mixing leading to the critical mixing temperatures of 694±55, 535±140, and 479±63 °C respectively. Spessartite would mix with almandine nearly ideally, and with grossularite with small positive deviation from ideality. The quarternary solution reduces essentially to a ternary mixture of pyrope, grossularite, and almandine + spessartite. The solid solubility relation, and tie line coordinates in this ternary system has been calculated as a function of temperature; the solid solution is found to be intrinsically stable for practically all ternary compositions at 600 °C.

Original languageEnglish (US)
Pages (from-to)137-148
Number of pages12
JournalContributions to Mineralogy and Petrology
Volume48
Issue number2
DOIs
StatePublished - Jun 1974
Externally publishedYes

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Garnets
aluminosilicate
solid solution
garnets
almandine
Solid solutions
garnet
solid solutions
energetics
pyrope
Ternary systems
ternary systems
Free energy
solubility
Solubility
temperature
free energy
crystal
deviation
Temperature

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology

Cite this

The energetics of natural garnet solid solution - I. Mixing of the aluminosilicate end-members. / Ganguly, Jibamitra; Kennedy, George C.

In: Contributions to Mineralogy and Petrology, Vol. 48, No. 2, 06.1974, p. 137-148.

Research output: Contribution to journalArticle

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