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Internally consistent solution models for Fe-Mg-Mn-Ti oxides; Fe-Ti oxides
David J. Andersen and Donald H. Lindsley
Internally consistent solution models for Fe-Mg-Mn-Ti oxides; Fe-Ti oxides
American Mineralogist (August 1988) 73 (7-8): 714-726
Internally consistent solution models for Fe-Mg-Mn-Ti oxides; Fe-Ti oxides
American Mineralogist (August 1988) 73 (7-8): 714-726
Index Terms/Descriptors
- calibration
- coexisting minerals
- data processing
- experimental studies
- geologic barometry
- geologic thermometry
- ilmenite
- iron
- iron oxides
- linear programming
- magnetite
- mathematical models
- metals
- minerals
- miscibility gap
- oxides
- P-T conditions
- phase equilibria
- theoretical studies
- thermodynamic properties
- titanium
- Fe-Ti oxides
Abstract
A model for coexisting ilmenite (sub ss) -magnetite (sub ss) 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 olivine (sub ss) -ilmenite (sub ss) and olivine (sub ss) -magnetite (sub ss) and Fe-Mn exchange for ilmenite (sub ss) -garnet (sub ss) .
ISSN: 0003-004X
EISSN: 1945-3027
Coden: AMMIAY
Serial Title: American Mineralogist
Serial Volume: 73
Serial Issue: 7-8
Title: Internally consistent solution models for Fe-Mg-Mn-Ti oxides; Fe-Ti oxides
Affiliation: State Univ. N.Y., Dep. Earth and Space Sci.,
Stony Brook, NY,
United States
Pages: 714-726
Published: 198808
Text Language: English
Publisher: Mineralogical Society of America,
Washington, DC,
United States
References: 65
Accession Number: 1988-071164
Categories: Mineralogy of non-silicates
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 5 tables
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United KingdomTwickenhamUKUnited Kingdom
Update Code: 1988
