Conditions of Formation of Iron–Carbon Melt Inclusions in Garnet and Orthopyroxene under P-T Conditions of Lithospheric Mantle › Research Explorer

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Conditions of Formation of Iron–Carbon Melt Inclusions in Garnet and Orthopyroxene under P-T Conditions of Lithospheric Mantle

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

DOI

https://doi.org/10.1134/S0869591118060024
Final published version

Yu V. Bataleva
Yu N. Palyanov
Yu M. Borzdov
I. D. Novoselov
O. A. Bayukov
N. V. Sobolev

Original language	English
Pages (from-to)	565-574
Number of pages	10
Journal	Petrology
Volume	26
Issue number	6
DOIs	https://doi.org/10.1134/S0869591118060024
Publication status	Published - 1 Nov 2018

Research areas

diamond, graphite, high-pressure experiment, mantle metasomatism, mantle silicates, metal–carbon melt, СО-fluid, OXIDATION, EARTHS MANTLE, STABILITY, metal-carbon melt, PHYSICOCHEMICAL PARAMETERS, METALLIC IRON, MINERAL INCLUSIONS, PRESSURE, CO2-fluid, DIAMOND FORMATION, NITROGEN, GENERATION

OECD FOS+WOS

ID: 17410723