Experimental investigation of the formation of cordierite-orthopyroxene parageneses in pelitic rocks
- 1 June 1980
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 73 (1), 15-22
- https://doi.org/10.1007/bf00376257
Abstract
No abstract availableKeywords
This publication has 9 references indexed in Scilit:
- Fe-Mg cordierite stability in high-grade pelitic rocks based on experimental, theoretical, and natural observationsContributions to Mineralogy and Petrology, 1977
- Mutual compatibility relations of the Fe (super +2) -Mg-Al silicates at 800 degrees C and 3 kbAmerican Journal of Science, 1976
- The reaction sillimanite+biotite+quartz?cordierite +K-feldspar+H2O and partial melting in the system K2O-FeO-MgO-Al2O3-SiO2-H2OContributions to Mineralogy and Petrology, 1976
- Thermal stability and standard thermodynamic properties of synthetic 2M1-muscovite, KAl2[AlSi3O10(OH)2]Contributions to Mineralogy and Petrology, 1974
- Phase equilibria in high-grade metamorphism and partial melting of pelitic rocksAmerican Journal of Science, 1973
- Melting Reactions in the System NaAlSi3O8-KAlSi3O8-SiO2-H2O to 20 Kilobars Compared with Results for Other Feldspar-Quartz-H2O and H2O SystemsThe Journal of Geology, 1970
- Partial melting of common rocks as a possible source of cordierite-anthophyllite bearing assemblagesAmerican Journal of Science, 1968
- Staurolite Stability in a Part of the System Fe-Al-Si-O-HJournal of Petrology, 1968
- The granite system at pressures of 4 to 10 kilobarsJournal of Geophysical Research, 1964