FeMg partitioning between coexisting garnet and phengite at high pressure, and comments on a garnet-phengite geothermometer
- 1 October 1982
- Vol. 15 (4) , 253-266
- https://doi.org/10.1016/0024-4937(82)90017-2
Abstract
No abstract availableKeywords
This publication has 18 references indexed in Scilit:
- Caledonian Sm–Nd ages and a crustal origin for Norwegian eclogitesNature, 1980
- Evidence for structural changes in garnet caused by calcium substitutionContributions to Mineralogy and Petrology, 1980
- Mantle-equilibrated Orthopyroxene Eclogite Pods from the Basal Gneisses in the Selje District, Western NorwayJournal of Petrology, 1978
- Temperature and pressure dependence of Fe-Mg partitioning between garnet and phengite, with particular reference to eclogitesContributions to Mineralogy and Petrology, 1978
- Evidence of Precambrian continent–continent collision in Western NorwayNature, 1977
- Petrology of eclogites and surrounding schists from the Lyell highway—Collingwood river areaJournal of the Geological Society of Australia, 1976
- Experimental determination of the temperature and pressure dependence of the Fe-Mg partition coefficient for coexisting garnet and clinopyroxeneContributions to Mineralogy and Petrology, 1974
- Genetic relationship between eclogite and hornblende + plagioclase pegmatite in western NorwayLithos, 1972
- Synthesis and stability of micas in the system K2O-MgO-SiO2-H2O and their relations to phlogopiteContributions to Mineralogy and Petrology, 1971
- Empirical Correction Factors for the Electron Microanalysis of Silicates and OxidesThe Journal of Geology, 1968