The effect of oxygen fugacity on the olivine to wadsleyite transformation: Implications for remote sensing of mantle redox state at the 410 km seismic discontinuity

American Mineralogist

Volumn 94, Issue 7, 2009, Pages 872-882

  Frost, Daniel J ^a   Mccammon, Catherine A ^a  

^a UNIVERSITÄT BAYREUTH   (Germany)

Author keywords

Ferric iron; Multianvil; Seismic discontinuity; Transition zone

Indexed keywords

HIGH PRESSURE EFFECTS; IRON; IRON METALLOGRAPHY; MOLYBDENUM METALLOGRAPHY; OLIVINE; OXYGEN; REMOTE SENSING; RHENIUM COMPOUNDS; SEISMOLOGY; SILICON;

410-KM DISCONTINUITY; FERRIC IRON; HIGH-PRESSURE AND TEMPERATURES; MULTI ANVILS; OXIDIZING CONDITIONS; SEISMIC DISCONTINUITIES; SSBAUER SPECTROSCOPIES; TRANSITION ZONES;

IRON COMPOUNDS;

DISCONTINUITY; EXPERIMENTAL MINERALOGY; FUGACITY; HIGH PRESSURE; HIGH TEMPERATURE; IRON; MANTLE; OLIVINE; OXYGEN; REDOX CONDITIONS; REMOTE SENSING; RINGWOODITE; SEISMICITY; TRANSFORMATION; TRANSITION ZONE; WADSLEYITE;

EID: 68949137090     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am.2009.3094     Document Type: Article

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