Systematic iron isotope variations in mantle rocks and minerals: The effects of partial melting and oxygen fugacity

By H. Williams, A. Peslier, C. McCammon, A. Halliday, S. Levasseur, N. Teutsch, J. Burg. 2005

225 citations recorded by the source corpus.

Subfields: Geophysics

View Paper: https://www.semanticscholar.org/paper/203fe5d5a9aa17eb9675a36d6e1df8d63c7db650

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In Geophysics

1. N. Dauphas

Citations in the corpus

• Modes of planetary-scale Fe isotope fractionation (2006, background): “Most likely some peridotite samples have undergone mantle metasomatism [30] and changes in mantle oxygen fugacity during partial melting that affected their original Fe isotope composition [19].”
• Abyssal peridotites reveal the near-chondritic Fe isotopic composition of the Earth (2013, background): “Several studies have previously examined whether mantle melting at oceanic ridges can fractionate Fe isotope compositions of the solid residue relative to the mantle source (e.g., Weyer and Ionov, 2007; Williams et al., 2005, 2009).”