On the hydration of olivine in ultramafic rocks: Implications from Fe isotopes in serpentinites

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On the hydration of olivine in ultramafic rocks: Implications from Fe isotopes in serpentinites

© 2017 The behavior of Fe during serpentinization largely controls the potential for oxidation-reduction reactions and energy budget for serpentinite-hosted microbial communities. We present Fe isotope data for mineral separates from a partially serpentinized dunite from New Caledonia to understand...

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Bibliographic Details
Main Authors:	Scott, S., Sims, K., Frost, B., Kelemen, P., Evans, Katy, Swapp, S.
Format:	Journal Article
Published:	Pergamon 2017
Online Access:	http://hdl.handle.net/20.500.11937/56321

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