The effect of garnet cell volume on the distribution of Mg and Fe in garnet exchange equilibria
- 31 December 1972
- Vol. 5 (1) , 33-55
- https://doi.org/10.1016/0024-4937(72)90078-3
Abstract
No abstract availableKeywords
This publication has 13 references indexed in Scilit:
- Classification of eclogites in terms of physical conditions of their originPhysics of the Earth and Planetary Interiors, 1970
- Irregular distribution of iron and magnesium among coexisting biotite and garnetLithos, 1969
- Pyroxene-garnet equilibrium and the depth facies of eclogitesInternational Geology Review, 1968
- The join Mg2Si2O6-CaMgSi2O6at 30 kilobars pressure and its application to pyroxenes from kimberlitesJournal of Geophysical Research, 1966
- Eclogites and Eclogites: Their Differences and SimilaritiesGSA Bulletin, 1965
- Distribution of Fe, Mg, and Mn between Garnet and Biotite in Natural Mineral AssemblagesThe Journal of Geology, 1965
- The System MgSiO3--CaMgSi2O6Journal of Petrology, 1964
- Analysis of Equilibrium in Garnet-Biotite-Sillimanite Gneisses from QuebecJournal of Petrology, 1964
- Metamorphic Grade and Iron-Magnesium Distribution between Co-Existing Garnet-Biotite and Garnet-HornblendeGeological Magazine, 1962
- Chemical Study of Garnet, Biotite, and Hornblende from Gneisses of Southwestern Quebec, with Emphasis on Distribution of Elements in Coexisting MineralsThe Journal of Geology, 1959