Original paper
Iron isotopic fractionation between silicate mantle and metallic core at high pressure
Abstract
The +0.1‰ elevated 56Fe/54Fe ratio of terrestrial basalts relative to chondrites was proposed to be a fingerprint of core-mantle segregation. However, the extent of iron isotopic fractionation between molten metal and silicate under high pressure-temperature conditions is poorly known. Here we show that iron forms chemical bonds of similar strengths in basaltic glasses and iron-rich alloys, even at high pressure. From the measured mean force...
Paper Details
Title
Iron isotopic fractionation between silicate mantle and metallic core at high pressure
Published Date
Feb 20, 2017
Journal
Volume
8
Issue
1
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Notes
History