Oxidation state of iron in hydrous mantle phases: Implications for subduction and mantle oxygen fugacity

Physics of the Earth and Planetary Interiors

Volumn 143, Issue 1-2, 2004, Pages 157-169

  McCammon, C A ^a   Frost, D J ^a   Smyth, J R ^b   Laustsen, H M S ^b   Kawamoto, T ^c   Ross, N L ^d   van Aken, P A ^e  

^a UNIVERSITÄT BAYREUTH   (Germany)

^b UNIVERSITY OF COLORADO   (United States)

^c KYOTO UNIVERSITY   (Japan)

^d VIRGINIA POLYTECHNIC INSTITUTE AND STATE UNIVERSITY   (United States)

^e DARMSTADT UNIVERSITY OF TECHNOLOGY   (Germany)

Author keywords

Ferric iron; M ssbauer spectroscopy; Subduction; Water

Indexed keywords

IRON; MAJORITE; MANTLE CHEMISTRY; OLIVINE; P-T CONDITIONS; RINGWOODITE; SUBDUCTION; WADSLEYITE;

EID: 2442494962     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2003.08.009     Document Type: Article

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