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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 and accretion

✍ Scribed by Franck Poitrasson; Mathieu Roskosz; Alexandre Corgne


Book ID
116453101
Publisher
Elsevier Science
Year
2009
Tongue
English
Weight
804 KB
Volume
278
Category
Article
ISSN
0012-821X

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