Effect of SiO2, total FeO, Fe3+/Fe2+ and alkali elements in basaltic glasses on mid-infrared spectra

American Mineralogist

Volumn 94, Issue 11-12, 2009, Pages 1580-1590

  Dufresne, Céleste D M ^a   King, Penelope L ^a,b   Dyar, M Darby ^c   Dalby, Klm N ^a  

^a UNIVERSITY OF WESTERN ONTARIO   (Canada)

^b UNIVERSITY OF NEW MEXICO   (United States)

^c MOUNT HOLYOKE COLLEGE   (United States)

Author keywords

Glass composition; IR peak location and shape; M ssbauer spectroscopy; Oxygen fugacity

Indexed keywords

ALUMINUM ALLOYS; ALUMINUM COMPOUNDS; BASALT; ELECTRON PROBE MICROANALYSIS; FOURIER TRANSFORM INFRARED SPECTROSCOPY; INFRARED DEVICES; IRON METALLOGRAPHY; IRON OXIDES; LOCATION; MOLYBDENUM METALLOGRAPHY; SILICA; SILICATES; SILICON; SODIUM COMPOUNDS;

ASYMMETRIC STRETCHING; COMPOSITIONAL CHANGES; FULL WIDTH HALF MAXIMUM; GLASS COMPOSITIONS; KRAMERS-KRONIG TRANSFORMS; MID-INFRARED SPECTRA; OXYGEN FUGACITY; SSBAUER SPECTROSCOPIES;

GLASS;

CHEMICAL COMPOSITION; ELECTRON PROBE ANALYSIS; FTIR SPECTROSCOPY; FUGACITY; GLASS; IRON OXIDE; MINERALOGY; MOSSBAUER SPECTROSCOPY; OXYGEN; SILICON;

EID: 77249128412     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am.2009.3113     Document Type: Article

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