High water contents in the Siberian cratonic mantle linked to metasomatism: An FTIR study of Udachnaya peridotite xenoliths

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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...

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Bibliographic Details
Main Authors:	Doucet, Luc-Serge, Peslier, A., Ionov, D., Brandon, A., Golovin, A., Goncharov, A., Ashchepkov, I.
Format:	Journal Article
Published:	Pergamon 2014
Online Access:	http://hdl.handle.net/20.500.11937/67234

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