Constraints on the form of the P-T loop in the Southern Marginal Zone of the Limpopo Belt, South Africa
- 1 March 1992
- journal article
- Published by Elsevier in Precambrian Research
- Vol. 55 (1-4) , 279-296
- https://doi.org/10.1016/0301-9268(92)90028-m
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- Thermobarometry and P-T paths from granulite facies rocks: an introductionPublished by Elsevier ,2003
- Constraints on the composition of fluids involved in retrograde anthophyllite formation in the Limpopo Belt, South AfricaPrecambrian Research, 1992
- The Granulite Uncertainty Principle: Limitations on Thermobarometry in GranulitesThe Journal of Geology, 1989
- Fluid-absent (dehydration) melting of biotite in metapelites in the early stages of crustal anatexisContributions to Mineralogy and Petrology, 1988
- Origin and evolution of granulites in normal and thickened crustsGeology, 1987
- PT-system, TX-system, PX-system: Three programs which calculate pressure-temperature-composition phase diagramsComputers & Geosciences, 1986
- Beginning of melting in the granite system Qz-Or-Ab-An-H2OContributions to Mineralogy and Petrology, 1984
- Experimental study of the stability of cordierite and garnet in pelitic compositions at high pressures and temperaturesContributions to Mineralogy and Petrology, 1973
- Stability of andalusite and the aluminum silicate phase diagramAmerican Journal of Science, 1971
- Theoretical phase relations involving cordierite and garnet in the system MgO-FeO-Al2O3-SiO2Contributions to Mineralogy and Petrology, 1971