The crystal/melt partitioning of V during mantle melting as a function of oxygen fugacity compared with some other elements (Al, P, Ca, Sc, Ti, Cr, Fe, Ga, Y, Zr and Nb)

Journal of Petrology

Volumn 50, Issue 9, 2009, Pages 1765-1794

  Mallmann, Guilherme ^a   O'Neill, Hugh St C ^a  

^a AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

Mantle; Oxygen fugacity; Partition coefficient; Redox state; Vanadium

Indexed keywords

ASTHENOSPHERE; FUGACITY; INDUCTIVELY COUPLED PLASMA METHOD; MANTLE CHEMISTRY; OXIDATION; OXYGEN; PARTIAL MELTING; PARTITION COEFFICIENT; REDOX CONDITIONS; SILICATE MELT; THERMODYNAMICS; TRACE ELEMENT; UPPER MANTLE; VANADIUM;

EID: 70349577509     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egp053     Document Type: Article

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