No iron isotope fractionation between molten alloys and...

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

Franck Poitrasson, Mathieu Roskosz, Alexandre Corgne
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Volume:
278
Year:
2009
Language:
english
DOI:
10.1016/j.epsl.2008.12.025
File:
PDF, 804 KB
english, 2009
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