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...
| Main Authors: | , , , |
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| Format: | Journal Article |
| Published: |
Wiley-Blackwell Publishing
2017
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| Online Access: | http://hdl.handle.net/20.500.11937/58965 |