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Lattard, Dominique, Le Breton, Nicole (1994) The P-T-fO 2 stability of deerite, Fe 12 2+ Fe 6 3+ [Si12O40](OH)10. Contributions to Mineralogy and Petrology, 115 (4) 474-487 doi:10.1007/bf00320980

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Reference TypeJournal (article/letter/editorial)
TitleThe P-T-fO 2 stability of deerite, Fe 12 2+ Fe 6 3+ [Si12O40](OH)10
JournalContributions to Mineralogy and Petrology
AuthorsLattard, DominiqueAuthor
Le Breton, NicoleAuthor
Year1994 (February)Volume115
Issue4
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf00320980Search in ResearchGate
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Mindat Ref. ID77019Long-form Identifiermindat:1:5:77019:4
GUID0
Full ReferenceLattard, Dominique, Le Breton, Nicole (1994) The P-T-fO 2 stability of deerite, Fe 12 2+ Fe 6 3+ [Si12O40](OH)10. Contributions to Mineralogy and Petrology, 115 (4) 474-487 doi:10.1007/bf00320980
Plain TextLattard, Dominique, Le Breton, Nicole (1994) The P-T-fO 2 stability of deerite, Fe 12 2+ Fe 6 3+ [Si12O40](OH)10. Contributions to Mineralogy and Petrology, 115 (4) 474-487 doi:10.1007/bf00320980
In(1994, February) Contributions to Mineralogy and Petrology Vol. 115 (4) Springer Science and Business Media LLC

See Also

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Langer, K., Lattard, D., Schreyer, W. (1977) Synthesis and stability of deerite, Fe2+12Fe3+6[Si12O40](OH)10, and Fe3+⇋Al3+ substitutions at 15–28 kb. Contributions to Mineralogy and Petrology, 60 (3) 271-297 doi:10.1007/bf01166801
Lattard, Dominique, Schreyer, Werner (1983) Synthesis and stability of the garnet calderite in the system Fe-Mn-Si-O. Contributions to Mineralogy and Petrology, 84 (2) 199-214 doi:10.1007/bf00371286
Lattard, Dominique (1987) Subsolidus phase relations in the system Zr-Fe-Ti-O in equilibrium with metallic iron. Implications for lunar petrology. Contributions to Mineralogy and Petrology, 97 (2) 264-278 doi:10.1007/bf00371245
Le Breton, Nicole (1989) Infrared investigation of CO2-bearing cordierites. Contributions to Mineralogy and Petrology, 103 (3) 387-396 doi:10.1007/bf00402923
Lattard, Dominique, Sauerzapf, Ursula, Käsemann, Martin (2005) New calibration data for the Fe–Ti oxide thermo-oxybarometers from experiments in the Fe–Ti–O system at 1 bar, 1,000–1,300°C and a large range of oxygen fugacities. Contributions to Mineralogy and Petrology, 149 (6) 735-754 doi:10.1007/s00410-005-0679-2
Holdaway, M. J. (1972) Thermal stability of Al-Fe epidote as a function of $$f_{{\text{o}}_{\text{2}} } $$ and Fe content. Contributions to Mineralogy and Petrology, 37 (4) 307-340 doi:10.1007/bf00371011
Breton, Nicole Le, Thompson, Alan Bruce (1988) Fluid-absent (dehydration) melting of biotite in metapelites in the early stages of crustal anatexis. Contributions to Mineralogy and Petrology, 99 (2) 226-237 doi:10.1007/bf00371463
Snyder, Don, Carmichael, Ian S. E., Wiebe, R. A. (1993) Experimental study of liquid evolution in an Fe-rich, layered mafic intrusion: constraints of Fe-Ti oxide precipitation on the T-fO 2 and T-? paths of tholeiitic magmas. Contributions to Mineralogy and Petrology, 113 (1) 73-86 doi:10.1007/bf00320832
(1994) Erratum. Contributions to Mineralogy and Petrology, 115 (3) 367 doi:10.1007/bf00310775
Woodland, Alan B., O’Neill, Hugh St. C. (1995) Phase relations between Ca3Fe 2 3 +Si3O12-Fe 3 2 +Fe 2 3 +Si3O12 garnet and CaFeSi2O6-Fe2Si2O6 pyroxene solid solutions. Contributions to Mineralogy and Petrology, 121 (1) 87-98 doi:10.1007/s004100050091
Sack, Richard O., Ghiorso, Mark S. (1991) An internally consistent model for the thermodynamic properties of Fe?Mg-titanomagnetite-aluminate spinels. Contributions to Mineralogy and Petrology, 106 (4) 474-505 doi:10.1007/bf00321989
 
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