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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

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Reference TypeJournal (article/letter/editorial)
TitleThe compositions of coexisting pyroxenes and garnet in the system CaO-MgO-Al2O3-SiO2 at 900°–1,100°C and high pressures
JournalContributions to Mineralogy and Petrology
AuthorsPerkins, DexterAuthor
Newton, Robert C.Author
Year1981 (September)Volume75
Issue3
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf01166769Search in ResearchGate
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Mindat Ref. ID75085Long-form Identifiermindat:1:5:75085:3
GUID0
Full ReferencePerkins, 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
Plain TextPerkins, 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
In(1981, September) Contributions to Mineralogy and Petrology Vol. 75 (3) Springer Science and Business Media LLC

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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
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
III, Dexter Perkins (1983) The stability of Mg-rich garnet in the system CaO-MgO-Al2O3-SiO2 at 1000-1300°C and high pressure. American Mineralogist, 68 (3-4) 355-364
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
Hansen, Birger (1981) The transition from pyroxene granulite facies to garnet clinopyroxene granulite facies. Experiments in the system CaO-MgO-Al2O3-SiO2. Contributions to Mineralogy and Petrology, 76 (2) 234-242 doi:10.1007/bf00371963
Koons, Peter O. (1982) An experimental investigation of the behavior of amphibole in the system Na2O-MgO-Al2O3-SiO2-H2O at high pressures. Contributions to Mineralogy and Petrology, 79 (3) 258-267 doi:10.1007/bf00371517
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
YAMADA, Hirohisa, TAKAHASHI, Eiichi (1984) Subsolidus Phase Relations Between Coexisting Garnet and Two Pyroxenes at 50 to 100 Kbar in the System CaO-MgO-Al2O3-SiO2. In Developments in Petrology. Elsevier. p.247-255. doi:10.1016/b978-0-444-42274-3.50026-3
Hensen, B. J. (1971) Theoretical phase relations involving cordierite and garnet in the system MgO-FeO-Al2O3-SiO2. Contributions to Mineralogy and Petrology, 33 (3) 191-214 doi:10.1007/bf00374063
Wood, Marcus I., Hess, Paul C. (1980) The structural role of Al2O3 and TiO2 in immiscible silicate liquids in the system SiO2-MgO-CaO-FeO-TiO2-Al2O3. Contributions to Mineralogy and Petrology, 72 (3) 319-328 doi:10.1007/bf00376151
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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