High water contents in the Siberian cratonic mantle linked to metasomatism: An FTIR study of Udachnaya peridotite xenoliths
The processes that control water distribution in nominally anhydrous minerals from peridotites are twofold. Melt depletion will remove water while metasomatism can potentially add water to these minerals. These processes can lead to a wide range of outcomes in water contents, which in turn could pla...
| Main Authors: | , , , , , , |
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| Format: | Journal Article |
| Published: |
Pergamon
2014
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| Online Access: | http://hdl.handle.net/20.500.11937/67234 |