High-pressure polymorphism of Fe2P and its implications for meteorites and Earth's core

Geophysical Research Letters

Volumn 35, Issue 10, 2008, Pages

  Dera, Przemyslaw ^a   Lavina, Barbara ^a   Borkowski, Lauren A ^a   Prakapenka, Vitali B ^a   Sutton, Stephen R ^a   Rivers, Mark L ^a   Downs, Robert T ^b   Boctor, Nabil Z ^c   Prewitt, Charles T ^b  

^a ARGONNE NATIONAL LABORATORY   (United States)

^b The University of Arizona   (United States)

^c GEOPHYSICAL LABORATORY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CONDENSATION; METEORITES; MINERALOGY; PHASE TRANSITIONS; PHOSPHORUS COMPOUNDS;

AMBIENT CONDITIONS; CHONDRITIC METEORITES; CONDENSATION PROCESSES; EARTH'S CORES; EQUILIBRIUM CONDENSATIONS; HIGH TEMPERATURES; PARENT BODIES; PHASE PRESENTS; PURE IRONS; ROOM TEMPERATURES; TYPE STRUCTURES; X-RAY DIFFRACTIONS;

MINERALS;

CHONDRITE; CORE (PLANETARY); HIGH PRESSURE; IRON; METEORITE; PHASE TRANSITION; POLYMORPHISM; X-RAY DIFFRACTION;

EID: 52949087506     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2008GL033867     Document Type: Article

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