An experimental study of the oxidation state of vanadium in spinel and basaltic melt with implications for the origin of planetary basalt

American Mineralogist

Volumn 91, Issue 10, 2006, Pages 1643-1656

  Richter, K ^a   Sutton, S R ^b,c   Newville, M ^c   Le, L ^a,d   Schwandt, C S ^d   Uchida, H ^e   Lavina, B ^f   Downs, R T ^e  

^a NASA JOHNSON SPACE CENTER   (United States)

^b UNIVERSITY OF CHICAGO   (United States)

^c UNIVERSITY OF CHICAGO   (United States)

^d JACOBS TECHNOLOGY   (United States)

^e University of Arizona   (United States)

^f UNIVERSITY OF PADOVA   (Italy)

Author keywords

Basalt; Oxygen fugacity; Spinel; Vanadium

Indexed keywords

BASALT; BINARY ALLOYS; GLASS; GLASS INDUSTRY; IRON ALLOYS; MAGNETITE; OXIDATION; OXYGEN; SILICATES; STRUCTURAL GEOLOGY; TITANIUM; VANADIUM;

CONSTANT TEMPERATURE; EXCHANGE EQUILIBRIA; METAL FRACTIONATION; NATURAL SYSTEMS; OXIDATION STATE; OXYGEN FUGACITY; PARTITION COEFFICIENT; SPINEL;

IRON COMPOUNDS;

BASALT; EXPERIMENTAL STUDY; FUGACITY; MELT; OXIC CONDITIONS; SPINEL; VANADIUM; XANES SPECTROSCOPY;

EID: 33845651748     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am.2006.2111     Document Type: Article

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