The role of sphene as an accessory phase in the high-pressure partial melting of hydrous mafic compositions
- 1 February 1979
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 42 (2) , 191-201
- https://doi.org/10.1016/0012-821x(79)90024-4
Abstract
No abstract availableKeywords
This publication has 30 references indexed in Scilit:
- Rare earth elements in carbonatite and cogenetic alkaline rocks: Examples from Seabrook Lake and Callander Bay, OntarioContributions to Mineralogy and Petrology, 1977
- Andesites and high-alumina basalts from the central-south Chile high Andes: Geochemical evidence bearing on their petrogenesisContributions to Mineralogy and Petrology, 1977
- The stability of sphene; experimental redetermination and geologic implicationsGeochimica et Cosmochimica Acta, 1977
- Role of underthrust oceanic crust in the genesis of a Fijian calc-alkaline suiteContributions to Mineralogy and Petrology, 1974
- Eclogites from Southwestern OregonGSA Bulletin, 1973
- The mineralogy of the glaucophane schists and associated rocks from le de Groix, Brittany, FranceContributions to Mineralogy and Petrology, 1972
- Iron-titanium oxides and oxygen fugacities in volcanic rocksJournal of Geophysical Research, 1967
- Eclogites and Eclogites: Their Differences and SimilaritiesGSA Bulletin, 1965
- Trachytes and their feldspar phenocrystsMineralogical Magazine and Journal of the Mineralogical Society, 1965
- The aegirine-granulites of Glen Lui, Braemar, AberdeenshireMineralogical Magazine and Journal of the Mineralogical Society, 1951