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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

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Reference TypeJournal (article/letter/editorial)
TitleExperimental 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
JournalContributions to Mineralogy and Petrology
AuthorsJenkins, D. M.Author
Newton, R. C.Author
Year1979Volume68
Issue4
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf01164525Search in ResearchGate
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Mindat Ref. ID74771Long-form Identifiermindat:1:5:74771:6
GUID0
Full ReferenceJenkins, 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
Plain TextJenkins, 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
In(1979) Contributions to Mineralogy and Petrology Vol. 68 (4) Springer Science and Business Media LLC

See Also

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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
Perkins, Dexter, Newton, Robert C. (1981) The compositions of coexisting pyroxenes and garnet in the system CaO-MgO-Al2O3-SiO2 at 900°–1,100°C and high pressures. Contributions to Mineralogy and Petrology, 75 (3) 291-300 doi:10.1007/bf01166769
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
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
Bertrand, P., Sotin, C., Mercier, J.-C. C., Takahashi, E. (1986) From the simplest chemical system to the natural one: garnet peridotite barometry. Contributions to Mineralogy and Petrology, 93 (2) 168-178 doi:10.1007/bf00371318
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
Frick, C. (1973) The sulphides in griquaite and garnet-peridotite xenoliths in kimberlite. Contributions to Mineralogy and Petrology, 39 (1) 1-16 doi:10.1007/bf00374242
MacGregor, Ian D. (1974) The system MgO-Al2O3-SiO2: Solubility of Al2O3 in enstatite for spinel and garnet peridotite compositions. American Mineralogist, 59 (1-2) 110-119
Carswell, D.A. (1968): Picritic magmaresidual dunite relationships in garnet peridotite at Kalskaret near Tafjord, South Norway. Contributions to Mineralogy and Petrology. 19, 97-124 (with analysis of olivine and pyrope fra Kalskaret]
Adams, Gerald E., Bishop, Finley C. (1986) The olivine ? clinopyroxene geobarometer: experimental results in the CaO-FeO-MgO-SiO2 system. Contributions to Mineralogy and Petrology, 94 (2) 230-237 doi:10.1007/bf00592939
Pattison, D. R. M., Newton, R. C. (1989) Reversed experimental calibration of the garnet-clinopyroxene Fe ? Mg exchange thermometer. Contributions to Mineralogy and Petrology, 101 (1) 87-103 doi:10.1007/bf00387203
 
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