Partial melting of phlogopite-bearing synthetic spinel- and garnet-lherzolites
- 1 January 1975
- journal article
- Published by Elsevier in Physics and Chemistry of the Earth
- Vol. 9, 845-854
- https://doi.org/10.1016/0079-1946(75)90055-5
Abstract
No abstract availableKeywords
This publication has 7 references indexed in Scilit:
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- The stability of phlogopite + enstatite at high pressures; a model for micas in the interior of the EarthAmerican Journal of Science, 1972
- Garnet-peridotite stability and occurrence in crust and mantleContributions to Mineralogy and Petrology, 1971
- A comparison of gel and glass starting materials for phase equilibrium studiesMineralogical Magazine, 1969
- Kyanite-sillimanite equilibrium between 700 degrees and 1500 degrees CAmerican Journal of Science, 1968
- Stability of phlogopite at high pressures and possible presence of phlogopite in the earth's upper mantleEarth and Planetary Science Letters, 1967
- Effect of pressure on the melting of diopside, CaMgSi2O6, and albite, NaAlSi3O8, in the range up to 50 kilobarsJournal of Geophysical Research, 1963