The Fe–C–O–H–N system at 6.3–7.8 GPa and 1200–1400 °C › Research Explorer

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The Fe–C–O–H–N system at 6.3–7.8 GPa and 1200–1400 °C: implications for deep carbon and nitrogen cycles

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/s00410-018-1472-3
Final published version

Alexander G. Sokol
Anatoly A. Tomilenko
Taras A. Bul’bak
Alexey N. Kruk
Pavel A. Zaikin
Ivan A. Sokol
Yurii V. Seryotkin
Yury N. Palyanov

Original language	English
Article number	47
Number of pages	17
Journal	Contributions to Mineralogy and Petrology
Volume	173
Issue number	6
DOIs	https://doi.org/10.1007/s00410-018-1472-3
Publication status	Published - 1 Jun 2018

Research areas

Carbon, Fluid, Gas chromatography–mass spectrometry, Hydrocarbons, Mantle, Metal, Nitrogen, TERRESTRIAL CARBON, HIGH-PRESSURE, OXYGEN FUGACITY, EARTHS MANTLE, MAGMA OCEAN, Gas chromatography-mass spectrometry, SILICATE MELTS, METALLIC IRON, CORE FORMATION, PHASE-RELATIONS, DIAMOND CRYSTAL-GROWTH

OECD FOS+WOS

ID: 13595344