Highly oxidising fluids generated during serpentinite breakdown in subduction zones
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/s41598-017-09626-y.pdf
Reference43 articles.
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2. Li, J.-L., Gao, J., Klemd, R., John, T. & Wang, X.-S. Redox processes in subducting oceanic crust recorded by sulfide-bearing high-pressure rocks and veins (SW Tianshan, China). Contributions to Mineralogy and Petrology 171, doi:10.1007/s00410-016-1284-2 (2016).
3. Parkinson, I. J. & Arculus, R. J. The redox state of subduction zones: insights from arc-peridotites. Chemical Geology 160, 409–423 (1999).
4. Kelley, K. A. & Cottrell, E. Water and the Oxidation State of Subduction Zone Magmas. Science 325, 605–607 (2009).
5. Evans, K. A. The redox budget of subduction zones. Earth-Science Reviews 113, 11–32, doi: 10.1016/j.earscirev.2012.03.003 (2012).
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