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

Alexandre Corgne, Franck Poitrasson, Mathieu Roskosz

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Key concepts: Silicate, Fractionation, Metallurgy, Isotope, Mineralogy, Geochemistry, Geology, Materials science

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No iron isotope fractionation between molten alloys and silicate melt to 2000 °C and 7.7 GPa: Experimental evidence and implications for planetary differentiation — Research Paper | ScholarLens