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...
| Main Authors: | , , , , , |
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| Format: | Journal Article |
| Published: |
Pergamon
2017
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| Online Access: | http://hdl.handle.net/20.500.11937/56321 |