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Water contents of nominally anhydrous mantle minerals have significant influence on the mantle strength and change with magmatism and metasomatism. Measurements of water content in olivine from the cratonic mantle are therefore an important tool for deciphering deep mantle processes, both rheological and geochemical. Due to the fast eruption rate of kimberlites, peridotite xenoliths from kimberlites are the best samples to study the distribution of in-situ water contents in the cratonic lithospheric mantle.

Hydration of the lithospheric mantle in the northern Slave craton (Canada): constraints from combined FTIR and EBSD measurements on peridotite xenoliths