In-situ X-ray diffraction measurements of the γ-ε transition boundary of iron in an internally-heated diamond anvil cell

Earth and Planetary Science Letters

Volumn 282, Issue 1-4, 2009, Pages 252-257

  Komabayashi, Tetsuya ^a,b   Fei, Yingwei ^a   Meng, Yue ^c   Prakapenka, Vitali ^d  

^a GEOPHYSICAL LABORATORY   (United States)

^b TOKYO INSTITUTE OF TECHNOLOGY   (Japan)

^c CARNEGIE INSTITUTION OF WASHINGTON   (United States)

^d UNIVERSITY OF CHICAGO   (United States)

Author keywords

high pressure; in situ X ray diffraction; internally heated diamond anvil cell; iron; phase transition

Indexed keywords

FACE-CENTERED CUBIC STRUCTURES; HEATING SYSTEMS; HEXAGONAL CLOSE-PACKED; HIGH PRESSURE; HIGHER TEMPERATURES; IN-SITU SYNCHROTRONS; IN-SITU X-RAY DIFFRACTION; INTERNALLY-HEATED DIAMOND ANVIL CELL; LIQUID TRIPLE POINTS; PHASE IDENTIFICATIONS; PHASE-TRANSITION BOUNDARIES; PRESSURE DETERMINATIONS; SOLID-PHASE; THERMAL EQUATIONS; TRANSITION BOUNDARIES;

DIAMONDS; DIFFRACTION; EQUATIONS OF STATE; HEATING; HIGH PRESSURE ENGINEERING; TOOLS; X RAY DIFFRACTION; X RAY DIFFRACTION ANALYSIS;

PHASE TRANSITIONS;

DIAMOND ANVIL CELL; EQUATION OF STATE; HIGH PRESSURE; IRON; PHASE TRANSITION; X-RAY DIFFRACTION;

EID: 67349281943     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2009.03.025     Document Type: Article

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