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Geochemical Evidence for Participation of the Subducted Crust in the Process of Transformation of the Subcontinental Mantle in the Yakutian Diamondiferous Province
Authors:Shatsky  V. S.  Ragozin  A. L.  Kozmenko  O. A.  Denisenko  A. A.
Affiliation:1.Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, 630090, Novosibirsk, Russia
;2.Novosibirsk State University, 630090, Novosibirsk, Russia
;3.Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of Sciences, 664033, Irkutsk, Russia
;
Abstract:Doklady Earth Sciences - The data available indicate the complex evolution of deformed peridotites of mantle xenoliths, the P–T parameters of which indicate that they are fragments of the...
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