Phase transition boundary between B1 and B8 structures of FeO up to 210GPa

Physics of the Earth and Planetary Interiors

Volumn 179, Issue 3-4, 2010, Pages 157-163

  Ozawa, Haruka ^a   Hirose, Kei ^a,b   Tateno, Shigehiko ^a,b   Sata, Nagayoshi ^b   Ohishi, Yasuo ^c  

^a TOKYO INSTITUTE OF TECHNOLOGY   (Japan)

^b JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

^c JAPAN SYNCHROTRON RADIATION RESEARCH INSTITUTE   (Japan)

Author keywords

B1 structure; B8 structure; DAC; Hcp iron; Phase transition; X ray diffraction

Indexed keywords

B1 PHASE; B1 STRUCTURE; CLAPEYRON SLOPE; DAC; EXPERIMENTAL CONDITIONS; HEXAGONAL CLOSE-PACKED IRONS; HIGH PRESSURE; IN-SITU; INNER CORE; LASER-HEATED DIAMOND-ANVIL CELL; MANTLE GEOTHERM; PHASE-TRANSITION BOUNDARY; PRESSURE RANGES; SOLID IRON; SYNCHROTRON X RAY DIFFRACTION;

DIGITAL INTEGRATED CIRCUITS; IRON OXIDES; METAL RECOVERY; OXYGEN; SODIUM CHLORIDE; X RAY DIFFRACTION;

PHASE TRANSITIONS;

CHEMICAL ANALYSIS; DIAMOND ANVIL CELL; HIGH PRESSURE; HIGH TEMPERATURE; IRON OXIDE; NICKEL; PHASE TRANSITION; SODIUM CHLORIDE; X-RAY DIFFRACTION;

EID: 77951091155     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2009.11.005     Document Type: Article

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