Data on the binary mixing properties of the (Fe,Mg,Ca)3Al2Si3O12 garnets and on the Fe-Mg partitioning between garnet and coexisting phases are reviewed, refined and critically analysed. Implications for certain multicomponent and thermobarometric calculations are discussed. -J.A.Z.
|Original language||English (US)|
|Number of pages||10|
|State||Published - Jan 1 1984|
ASJC Scopus subject areas
- Geochemistry and Petrology