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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, 107 (3) 415 doi:10.1007/bf00325108

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Reference TypeJournal (article/letter/editorial)
TitleAn internally consistent model for the thermodynamic properties of Fe-Mg-titanomagnetite-aluminate spinels
JournalContributions to Mineralogy and Petrology
AuthorsSack, Richard O.Author
Ghiorso, Mark S.Author
Year1991 (May)Volume107
Issue3
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf00325108Search in ResearchGate
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Mindat Ref. ID76635Long-form Identifiermindat:1:5:76635:9
GUID0
Full ReferenceSack, 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, 107 (3) 415 doi:10.1007/bf00325108
Plain TextSack, 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, 107 (3) 415 doi:10.1007/bf00325108
In(1991, May) Contributions to Mineralogy and Petrology Vol. 107 (3) Springer Science and Business Media LLC

See Also

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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
Sack, Richard O., Ghiorso, Mark S. (1989) Importance of considerations of mixing properties in establishing an internally consistent thermodynamic database: thermochemistry of minerals in the system Mg2SiO4-Fe2SiO4-SiO2. Contributions to Mineralogy and Petrology, 102 (1) 41-68 doi:10.1007/bf01160190
Ghiorso, Mark S., Sack, Richard O. (1995) Chemical mass transfer in magmatic processes IV. A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures. Contributions to Mineralogy and Petrology, 119 (2) 197-212 doi:10.1007/bf00307281
Ghiorso, Mark S., Sack, O. (1991) Fe-Ti oxide geothermometry: thermodynamic formulation and the estimation of intensive variables in silicic magmas. Contributions to Mineralogy and Petrology, 108 (4) 485-510 doi:10.1007/bf00303452
Sack, Richard O., Ghiorso, Mark S. (1998) Thermodynamics of feldspathoid solutions. Contributions to Mineralogy and Petrology, 130 (3) 256-274 doi:10.1007/s004100050364
Sack, Richard O., Ghiorso, Mark S. (1994) Thermodynamics of multicomponent pyroxenes: I. Formulation of a general model. Contributions to Mineralogy and Petrology, 116 (3) 277-286 doi:10.1007/bf00306497
Ghiorso, M. S., Sack, Richard O. (1995) Chemical mass transfer in magmatic processes IV. A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures. Contributions to Mineralogy and Petrology, 119 (2) 197-212 doi:10.1007/s004100050036
Sack, Richard O. (1980) Some constraints on the thermodynamic mixing properties of Fe-Mg orthopyroxenes and olivines. Contributions to Mineralogy and Petrology, 71 (3) 257-269 doi:10.1007/bf00371667
Ghosal, Subhabrata, Sack, Richard O., Ghiorso, Mark S., Lipschutz, Michael E. (1998) Evidence for a reduced, Fe-depleted martian mantle source region of shergottites. Contributions to Mineralogy and Petrology, 130 (3) 346-357 doi:10.1007/s004100050370
Sack, Richard O., Ghiorso, Mark S. (1994) Thermodynamics of multicomponent pyroxenes: II. Phase relations in the quadrilateral. Contributions to Mineralogy and Petrology, 116 (3) 287-300 doi:10.1007/bf00306498
Ghiorso, Mark S., Carmichael, Ian S. E., Rivers, Mark L., Sack, Richard O. (1983) The Gibbs free energy of mixing of natural silicate liquids; an expanded regular solution approximation for the calculation of magmatic intensive variables. Contributions to Mineralogy and Petrology, 84 (2) 107-145 doi:10.1007/bf00371280
 
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