(Q57885915)

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

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H2O in olivine and garnet inclusions still trapped in diamonds from the Siberian craton: Implications for the water content of cratonic lithosphere peridotites (English)
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Nathalie Bolfan-Casanova
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Jeffrey W. Harris
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August 2015
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230
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180-183
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