Redox equilibria of iron in alkaline earth silicate melts; relationships between melt structure, oxygen fugacity, temperature and properties of iron-bearing silicate liquids

Mossbauer and Raman spectroscopy have been used to relate redox equilibria of iron to melt structure in MO-SiO2 systems (M = Ba2+, Sr2+, Ca2+, Mg2+).

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Bibliographic Details
Published inThe American mineralogist Vol. 69; no. 9-10; pp. 834 - 847
Main Authors Mysen, Bjørn O, Virgo, David, Seifert, Friedrich A
Format Journal Article
LanguageEnglish
Published Mineralogical Society of America 01.10.1984
Subjects
experimental studies
fugacity
geochemistry
igneous and metamorphic rocks
iron
liquid structure
melting
metals
MO-SiO2 (M = Ba2+, Sr2+, Ca2+, Mg2+)
Mossbauer spectra
Petrology
phase equilibria
properties
Raman spectra
rock, sediment, soil
silicates
spectra
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Summary:Mossbauer and Raman spectroscopy have been used to relate redox equilibria of iron to melt structure in MO-SiO2 systems (M = Ba2+, Sr2+, Ca2+, Mg2+).
ISSN:0003-004X
1945-3027