Potassium partitioning into molten iron alloys at high-pressure: Implications for Earth's core

Physics of the Earth and Planetary Interiors

Volumn 160, Issue 1, 2007, Pages 22-33

  Bouhifd, M A ^a,b   Gautron, L ^c   Bolfan Casanova, N ^d   Malavergne, V ^c   Hammouda, T ^d   Andrault, D ^b   Jephcoat, A P ^a,e  

^a UNIVERSITY OF OXFORD   (United Kingdom)

^b INSTITUT DE PHYSIQUE DU GLOBE DE PARIS   (France)

^c UNIVERSITÉ GUSTAVE EIFFEL   (France)

^d UNIVERSITÉ CLERMONT AUVERGNE   (France)

^e DIAMOND LIGHT SOURCE LTD   (United Kingdom)

Author keywords

Chemical composition; Earth's core; High pressure; Iron alloy; Partition coefficients; Partitioning; Potassium

Indexed keywords

COMPOSITION; EARTH (PLANET); HIGH PRESSURE EFFECTS; LIQUID METALS; PHASE COMPOSITION; POTASSIUM;

EARTH'S CORE; PARTITION COEFFICIENTS; SILICATE MELT COMPOSITION; THERMAL BUDGET MODELS;

IRON ALLOYS;

CHEMICAL COMPOSITION; CORE (PLANETARY); FUGACITY; HIGH PRESSURE; HIGH TEMPERATURE; IRON; PARTITION COEFFICIENT; PARTITIONING; POTASSIUM; SANIDINE;

EID: 33845630767     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2006.08.005     Document Type: Article

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