Element Partitioning Between Magnesiowüstite and Silicate Melt as a Function of Melt Composition and Temperature at High Pressure

The influence of melt composition and temperature on the partitioning of siderophile elements between magnesiowustite (Mw) and silicate melt (Sil) has been studied systematically at 9 GPa. Additional experiments at pressures above 20 GPa were performed to determine the effect of pressure. The determ...

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Veröffentlicht in:	The Review of High Pressure Science and Technology 1998/03/03, Vol.7, pp.66-68
Hauptverfasser:	Geßmann, C. K., Ohtani, E., Rubie, D. C.
Format:	Artikel
Sprache:	eng
Schlagworte:	magma ocean magnesiowüstite fractionation mineral-melt partitioning siderophile element anomaly silicate melt composition
Online-Zugang:	Volltext
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