Solubility of hydrogen and ferric iron in rutile and TiO2 (II : Implications for phase assemblages during ultrahigh-pressure metamorphism and for the stability of silica polymorphs in the lower mantle

Geophysical Research Letters

Volumn 31, Issue 4, 2004, Pages

  Bromiley, Geoffrey ^a   Hilaret, Nadège ^b   McCammon, Catherine ^a  

^a UNIVERSITÄT BAYREUTH   (Germany)

^b UNIVERSITÉ DE LYON   (France)

Author keywords

[No Author keywords available]

Indexed keywords

COUPLED CIRCUITS; DEHYDRATION; HYDROGEN; IRON COMPOUNDS; OXYGEN; SUBSTITUTION REACTIONS; TITANIUM OXIDES;

FERRIC IRON; OCEANIC CRUST; RUTILE; SUBDUCTION;

SOLUBILITY;

HYDROGEN; IRON; LOWER MANTLE; PHASE TRANSITION; RUTILE; SOLUBILITY; ULTRAHIGH PRESSURE METAMORPHISM;

EID: 2542418931     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2004GL019430     Document Type: Article

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