Interaction of peridotite with Ca-rich carbonatite melt at 3.1 and 6.5 GPa › Research Explorer

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Interaction of peridotite with Ca-rich carbonatite melt at 3.1 and 6.5 GPa: Implication for merwinite formation in upper mantle, and for the metasomatic origin of sublithospheric diamonds with Ca-rich suite of inclusions

Research output: Contribution to journal › Article › peer-review

Laboratory for Experimental Geochemistry and Petrology of the Earth's Mantle

DOI

https://doi.org/10.1007/s00410-017-1432-3
Final published version

Igor S. Sharygin
Anton Shatskiy
Konstantin D. Litasov
Alexander V. Golovin
Eiji Ohtani
Nikolay P. Pokhilenko

Original language	English
Article number	22
Number of pages	16
Journal	Contributions to Mineralogy and Petrology
Volume	173
Issue number	3
DOIs	https://doi.org/10.1007/s00410-017-1432-3
Publication status	Published - 1 Mar 2018

Research areas

Carbonatite melt, Diamond, Mantle, Merwinite, Subduction, HIGH-PRESSURE, UDACHNAYA-EAST KIMBERLITE, DEEP MANTLE, ECLOGITE, EARTHS INTERIOR, CONTINENTAL LITHOSPHERIC MANTLE, TRANSPORT, EXTRACTION, TRANSITION ZONE, PHASE-RELATIONS

OECD FOS+WOS

ID: 10422101