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Highly oxidising fluids generated during serpentinite breakdown in subduction zones.

B Debret1,2, D A Sverjensky3

  • 1Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK. ba.debret@gmail.com.

Scientific Reports
|September 6, 2017
PubMed
Summary

Fluids released from dehydrating serpentinite in subduction zones are highly oxidizing, explaining the oxidized lavas and gas emissions from arc volcanism. This process influences Earth

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