Internally consistent solution models for Fe-Mg-Mn-Ti oxides; Fe-Ti oxides

A model for coexisting ilmenitess-magnetitess based on new and existing experimental data for the Fe-Ti oxides is developed using linear programming. The model is internally consistent with the available data for Fe-Mg exchange for oliviness-ilmenitess and oliviness-magnetitess and Fe-Mn exchange fo...

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Bibliographische Detailangaben
Veröffentlicht in:	The American mineralogist 1988-08, Vol.73 (7-8), p.714-726
Hauptverfasser:	Andersen, David J, Lindsley, Donald H
Format:	Artikel
Sprache:	eng
Schlagworte:	calibration coexisting minerals Condensed matter: structure, mechanical and thermal properties data processing Exact sciences and technology experimental studies Fe-Ti oxides geologic barometry geologic thermometry ilmenite Inorganic compounds iron iron oxides linear programming magnetite mathematical models metals Mineralogy minerals miscibility gap nonsilicates oxides P-T conditions phase equilibria Physics Structure of solids and liquids crystallography Structure of specific crystalline solids theoretical studies thermodynamic properties titanium Water, oxides, hydroxides, peroxides
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Beschreibung
Zusammenfassung:	A model for coexisting ilmenitess-magnetitess based on new and existing experimental data for the Fe-Ti oxides is developed using linear programming. The model is internally consistent with the available data for Fe-Mg exchange for oliviness-ilmenitess and oliviness-magnetitess and Fe-Mn exchange for ilmenitess-garnetss.
ISSN:	0003-004X 1945-3027