Theoretical phase relations involving cordierite and garnet in the system MgO-FeO-Al2O3-SiO2
- 1 January 1971
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 33 (3) , 191-214
- https://doi.org/10.1007/bf00374063
Abstract
No abstract availableKeywords
This publication has 8 references indexed in Scilit:
- Experimental data on coexisting cordierite and garnet under high grade metamorphic conditionsPublished by Elsevier ,2002
- Stability of pyrope-quartz in the system MgO-Al2O3-SiO2Contributions to Mineralogy and Petrology, 1971
- Low-temperature Compatibility Relations of Cordierite in Haplopelites of the System K2O--MgO--Al2O3--SiO2--H2OJournal of Petrology, 1970
- The metamorphic paragenesis of cordierite in pelitic rocksContributions to Mineralogy and Petrology, 1969
- Phase Relationships in the System Fe3Al2Si3O12-Mg3Al2Si3O12-H2O at 2.0 KilobarsGSA Bulletin, 1969
- Partial melting of common rocks as a possible source of cordierite-anthophyllite bearing assemblagesAmerican Journal of Science, 1968
- Ti in biotite and muscovite as an indication of metamorphic grade in almandine amphibolite facies rocks from Sudbury, OntarioGeochimica et Cosmochimica Acta, 1968
- Selected Phase Relationships in the System Al-Mn-Fe-Si-O-H: A Model for Garnet EquilibriaJournal of Petrology, 1968