The Fe-rich liquidus in the Fe–FeS system from 1 bar to 10 GPa

The composition and evolution of a metallic planetary core is determined by the behavior with pressure of the eutectic and the liquidus on the Fe-rich side of the Fe–FeS eutectic. New experiments at 6 GPa presented here, along with existing experimental data, inform a thermodynamic model for this li...

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Veröffentlicht in:	Geochimica et cosmochimica acta 2011-04, Vol.75 (8), p.2072-2087
Hauptverfasser:	Buono, Antonio S., Walker, David
Format:	Artikel
Sprache:	eng
Schlagworte:	Crystal structure Eutectic composition Eutectic temperature Evolution Iron Liquids Liquidus Pivots Thermodynamic models
Online-Zugang:	Volltext
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