The Si+4 content of natural phengites: A discussion
- 1 January 1968
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 17 (1), 78-81
- https://doi.org/10.1007/bf00371811
Abstract
No abstract availableKeywords
This publication has 7 references indexed in Scilit:
- The greenschist facies in part of eastern Otago, New ZealandContributions to Mineralogy and Petrology, 1967
- Si+4 Content of natural phengitesContributions to Mineralogy and Petrology, 1967
- The sillimanite-potash feldspar isograd in Western Maine, U.S.A.Contributions to Mineralogy and Petrology, 1966
- Composition of plagioclase and associated minerals in some schists from Vermont, U.S.A., and South Westland, New Zealand, with inferences about the peristerite solvusContributions to Mineralogy and Petrology, 1966
- Phengite micas; synthesis, stability, and natural occurrenceAmerican Journal of Science, 1965
- The Lower Greenschist Facies in the Scottish HighlandsGeologiska Föreningen i Stockholm Förhandlingar, 1965
- XXV.—The Mineralogy and Metamorphism of the Moine Schists of the Morar and Knoydart Districts of Inverness-shireTransactions of the Royal Society of Edinburgh, 1959