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Composition of reduced mantle fluids: Evidence from modeling experiments and fluid inclusions in natural diamond

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

DOI

https://doi.org/10.15372/RGG2020103
Final published version

A. G. Sokol
A. A. Tomilenko
T. A. Bul'bak
I. A. Sokol
P. A. Zaikin
N. V. Sobolev

Original language	English
Pages (from-to)	663-674
Number of pages	12
Journal	Russian Geology and Geophysics
Volume	61
Issue number	5-6
DOIs	https://doi.org/10.15372/RGG2020103
Publication status	Published - 1 May 2020

Research areas

Deep cycle of carbon, Fluid, Hydrocarbons, Inclusions in diamond, Mantle, Nitrogen, OXYGEN FUGACITY, P-T CONDITIONS, hydrocarbons, deep cycle of carbon and nitrogen, LITHOSPHERIC MANTLE, EARTHS MANTLE, VOLATILE COMPONENTS, inclusions in diamond, HIGH-PRESSURES, PERIDOTITE XENOLITHS, YAKUTIAN KIMBERLITES, mantle, O-H FLUID, fluid, SULFIDE INCLUSIONS

OECD FOS+WOS

ID: 24895105