A decompressional P–T path, Reinbolt Hills, East Antarctica
- 5 May 1991
- journal article
- Published by Wiley in Journal of Metamorphic Geology
- Vol. 9 (3) , 257-266
- https://doi.org/10.1111/j.1525-1314.1991.tb00521.x
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- Proterozoic Granulites from the Rauer Group, East Antarctica. I. Decompressional Pressure-Temperature Paths Deduced from Mafic and Felsic GneissesJournal of Petrology, 1988
- Internally-Consistent Thermodynamic Data for Minerals in the System Na2O-K2O-CaO-MgO-FeO-Fe2O3-Al2O3-SiO2-TiO2-H2O-CO2Journal of Petrology, 1988
- Ge0-calc: Software package for calculation and display of pressure-temperature-composition phase diagrams using an IBM or compatible personal computerComputers & Geosciences, 1988
- The mutual solubility of coexisting ortho- and clinopyroxene: toward an absolute geothermometer for the natural system?Earth and Planetary Science Letters, 1985
- An experimental study of the partitioning of Fe and Mg between garnet and orthopyroxeneContributions to Mineralogy and Petrology, 1984
- The Solubility of Alumina in Orthopyroxene Coexisting with Garnet in FeO-MgO--Al2O3--SiO2 and CaO--FeO--MgO--Al2O3--SiO2Journal of Petrology, 1984
- The Cordierite-Garnet-Sillimanite-Quartz Equilibrium: Experiments and ApplicationsPublished by Springer Nature ,1983
- Geobarometry in GranulitesPublished by Springer Nature ,1983
- Garnet–orthopyroxene barometry for granulites and peridotitesNature, 1982
- Experimental calibration of the partitioning of Fe and Mg between biotite and garnetContributions to Mineralogy and Petrology, 1978