Redistribution of Iron and Titanium in High-Pressure Ultramafic Rocks

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Redistribution of Iron and Titanium in High-Pressure Ultramafic Rocks

© 2017. American Geophysical Union. The redox state of iron in high-pressure serpentinites, which host a significant proportion of Fe 3+ in subduction zones, can be used to provide an insight into iron cycling and constrain the composition of subduction zone fluids. In this study, we use oxide and s...

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Bibliographic Details
Main Authors:	Crossley, R., Evans, Katy, Reddy, S., Lester, G.
Format:	Journal Article
Published:	Wiley-Blackwell Publishing 2017
Online Access:	http://hdl.handle.net/20.500.11937/58965

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