Effects of melt percolation on iron isotopic variation in peridotites from Yangyuan, North China Craton
Review articleOpen access

Highlights•Fe isotope ratios of two suites of mantle xenoliths from Yangyuan were measured.•Mg-lherzolites show a limited variation in Fe isotopic composition.•Fe-rich lherzolites exhibit extremely light Fe isotopic compositions.•Such variation appears to result from diffusion-driven kinetic isotope effects.

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