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Gasparik, T., Newton, R. C. (1984) The reversed alumina contents of orthopyroxene in equilibrium with spinel and forsterite in the system MgO-Al2O3-SiO2. Contributions to Mineralogy and Petrology, 85 (2) 186-196 doi:10.1007/bf00371708

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Reference TypeJournal (article/letter/editorial)
TitleThe reversed alumina contents of orthopyroxene in equilibrium with spinel and forsterite in the system MgO-Al2O3-SiO2
JournalContributions to Mineralogy and Petrology
AuthorsGasparik, T.Author
Newton, R. C.Author
Year1984 (February)Volume85
Issue2
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf00371708Search in ResearchGate
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Mindat Ref. ID75541Long-form Identifiermindat:1:5:75541:4
GUID0
Full ReferenceGasparik, T., Newton, R. C. (1984) The reversed alumina contents of orthopyroxene in equilibrium with spinel and forsterite in the system MgO-Al2O3-SiO2. Contributions to Mineralogy and Petrology, 85 (2) 186-196 doi:10.1007/bf00371708
Plain TextGasparik, T., Newton, R. C. (1984) The reversed alumina contents of orthopyroxene in equilibrium with spinel and forsterite in the system MgO-Al2O3-SiO2. Contributions to Mineralogy and Petrology, 85 (2) 186-196 doi:10.1007/bf00371708
In(1984, February) Contributions to Mineralogy and Petrology Vol. 85 (2) Springer Science and Business Media LLC

See Also

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Herzberg, Claude T. (1983) The reaction forsterite+cordierite=aluminous orthopyroxene+spinel in the system MgO-Al2O3-SiO2. Contributions to Mineralogy and Petrology, 84 (1) 84-90 doi:10.1007/bf01132333
Perkins, D., Holland, T. J. B., Newton, R. C. (1981) The Al2O3 contents of enstatite in equilibrium with garnet in the system MgO-Al2O3-SiO2 at 15–40 kbar and 900°–1,600° C. Contributions to Mineralogy and Petrology, 78 (1) 99-109 doi:10.1007/bf00371147
Gasparik, Tibor (1984) Two-pyroxene thermobarometry with new experimental data in the system CaO-MgO-Al2O3-SiO2. Contributions to Mineralogy and Petrology, 87 (1) 87-97 doi:10.1007/bf00371405
Mukhopadhyay, Biswajit (1991) Forsterite-diopside-spinel-liquid equilibria in the system CaO?MgO?Al2O3?SiO2 at 20 kbar and petrological applications. Contributions to Mineralogy and Petrology, 106 (2) 253-264 doi:10.1007/bf00306437
Danckwerth, P. A., Newton, R. C. (1978) Experimental determination of the spinel peridotite to garnet peridotite reaction in the system MgO-Al2O3-SiO2 in the range 900-1100 °C and Al2O3 isopleths of enstatite in the spinel field. Contributions to Mineralogy and Petrology, 66 (2). 189-201 doi:10.1007/bf00372158
Liermann, H. P., Ganguly, J. (2003) Fe2+–Mg fractionation between orthopyroxene and spinel: experimental calibration in the system FeO–MgO–Al2O3–Cr2O3–SiO2, and applications. Contributions to Mineralogy and Petrology, 145 (2) 217-227 doi:10.1007/s00410-003-0444-3
Jenkins, D. M., Newton, R. C. (1979) Experimental determination of the spinel peridotite to garnet peridotite inversion at 900� C and 1,000� C in the system CaO-MgO-Al2O3-SiO2, and at 900� C with natural garnet and olivine. Contributions to Mineralogy and Petrology, 68 (4) 407-419 doi:10.1007/bf01164525
Liermann, H. P., Ganguly, J. (2007) Fe2+–Mg fractionation between orthopyroxene and spinel: experimental calibration in the system FeO–MgO–Al2O3–Cr2O3–SiO2, and applications. Contributions to Mineralogy and Petrology, 154 (4) 491 doi:10.1007/s00410-007-0204-x
Annersten, H., Seifert, F. (1981) Stability of the assemblage orthopyroxene-sillimanite-quartz in the system MgO-FeO-Fe2O3-Al2O3-SiO2-H2O. Contributions to Mineralogy and Petrology, 77 (2) 158-165 doi:10.1007/bf00636519
HARLEY, S. L. (1984) The Solubility of Alumina in Orthopyroxene Coexisting with Garnet in FeO-MgO--Al2O3--SiO2 and CaO--FeO--MgO--Al2O3--SiO2. Journal of Petrology, 25 (3) 665-696 doi:10.1093/petrology/25.3.665
Farmer, Nicholas, O’Neill, Hugh St. C., Green, Eleanor C. R. (2025) The spinel to garnet phase transition in the systems MgO-Al2O3-SiO2 and CaO-MgO-Al2O3-SiO2: new experiments to resolve long-standing discrepancies. Contributions to Mineralogy and Petrology, 180 (2). doi:10.1007/s00410-025-02203-x
 
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