Garnet-spinel-olivine-orthopyroxene equilibria in the FeO-MgO-Al2O3-SiO2-Cr2O3 system: I. Composition and molar volumes of minerals

European Journal of Mineralogy

Volumn 11, Issue 4, 1999, Pages 599-617

  Brey, Gerhard P ^a   Doroshev, Alexei M ^b   Girnis, Andrei V ^a,c   Turkin, Alexandr I ^b  

^a GOETHE UNIVERSITY   (Germany)

^b SOBOLEV INSTITUTE OF GEOLOGY AND MINERALOGY   (Russian Federation)

^c INSTITUTE OF GEOLOGY OF ORE DEPOSITS   (Russian Federation)

Author keywords

Mantle mineralogy; Molar volume; Peridotite; Phase equilibrium; Solid solution

Indexed keywords

ALUMINA; ALUMINUM ALLOYS; ALUMINUM METALLOGRAPHY; ALUMINUM OXIDE; BINARY ALLOYS; CHROMIUM ALLOYS; DENSITY (SPECIFIC GRAVITY); GARNETS; IRON ALLOYS; IRON METALLOGRAPHY; IRON OXIDES; MAGNESIA; MAGNESIUM ALLOYS; MAGNESIUM METALLOGRAPHY; MIXING; OLIVINE; OXIDE MINERALS; PHASE EQUILIBRIA; SILICA; SOLID SOLUTIONS; VOLUME MEASUREMENT;

INITIAL COMPOSITION; MINERAL EQUILIBRIA; NEGATIVE DEVIATIONS; PERIDOTITE; PRESSURE AND TEMPERATURE; SPINEL PERIDOTITES; SYMMETRICAL MODELS; UNIT CELL PARAMETERS;

CHROMIUM METALLOGRAPHY;

MANTLE CHEMISTRY; PERIDOTITE; PHASE EQUILIBRIUM; SOLID SOLUTION;

EID: 0032711601     PISSN: 09351221     EISSN: None     Source Type: Journal    
DOI: 10.1127/ejm/11/4/0599     Document Type: Article

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