H2O in olivine and garnet inclusions still trapped in diamonds from the Siberian craton: Implications for the water content of cratonic lithosphere peridotites

Title
H2O in olivine and garnet inclusions still trapped in diamonds from the Siberian craton: Implications for the water content of cratonic lithosphere peridotites
Authors
Keywords
Diamond, Inclusion, Craton, Nominally anhydrous minerals, Water, FTIR
Journal
LITHOS
Volume 230, Issue -, Pages 180-183
Publisher
Elsevier BV
Online
2015-05-31
DOI
10.1016/j.lithos.2015.05.013

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