Article ISI
Earth and Planetary Science Letters  (2009)

No iron isotope fractionation between molten alloys and silicate melt to 2000°C and 7.7 GPa=> Experimental evidence and implications for planetary differentiation and accretion.

F. Poitrasson, M. Roskosz

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Título de la Revista: Earth and Planetary Science Letters
Fecha de publicación: 2009
DOI/URL:

10.1016/j.epsl.2008.12.025