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The phase relations in the FeO-MgO-Al2O3-SiO2 system: assessment of thermodynamic properties and phase equilibria at pressures up to 30 GPa
Uppsala University.
1999 (English)In: CALPHAD-COMPUTER COUPLING OF PHASE DIAGRAMS AND THERMOCHEMISTRY, ISSN 0364-5916, Vol. 23, no 1, 19-67 p.Article in journal (Other scientific) Published
Abstract [en]

Thermodynamic parameters for minerals in the FeO-MgO-Al2O3-SiO2 (FMAS) system have been assessed from phase equilibria at pressures up to 30 GPa. All solid solution phases except orthopyroxene have been described by the sublattice model. Calculated phase

Place, publisher, year, edition, pages
PERGAMON-ELSEVIER SCIENCE LTD , 1999. Vol. 23, no 1, 19-67 p.
Keyword [en]
REGULAR SOLUTION MODEL; EARTHS LOWER MANTLE; ORTHO-PYROXENE; GEOPHYSICAL IMPLICATIONS; (MG;FE)SIO3 PEROVSKITE; ELECTRON-MICROSCOPY; FEO-MGO-SIO2 SYSTEM; SILICATE PEROVSKITE; HIGH-TEMPERATURE; TRANSITION ZONE
Identifiers
URN: urn:nbn:se:uu:diva-27747OAI: oai:DiVA.org:uu-27747DiVA: diva2:55643
Note
Addresses: Fabrichnaya OB, Royal Inst Technol, Dept Mat Sci, S-10044 Stockholm, Sweden. Uppsala Univ, Inst Earth Sci, Theoret Geochem Program, SE-75236 Uppsala, Sweden.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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