Peculiarities of the Composition of Volatiles of Diamonds Synthesized in the Fe–S–C System: Data on Gas Chromatography–Mass Spectrometry


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The first chromatography–mass spectroscopy data on volatiles in diamonds synthesized in the Fe–S–C system with 5 wt % S at 1400–1450°C and 5.0–5.5 GPa indicate the evolution of volatile composition during the diamond growth and, correspondingly, the variation in redox conditions of the reaction cell. A significant role is played by various hydrocarbons (HCs) and their derivatives, the content of which can reach 87%. Our data on possible abiogenic synthesis of HCs (components of natural gas and oil) can result in global recalculations (including climate) related to the global C cycle.

Sobre autores

A. Tomilenko

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Autor responsável pela correspondência
Email: tomilen@igm.nsc.ru
Rússia, Novosibirsk, 630090

E. Zhimulev

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: tomilen@igm.nsc.ru
Rússia, Novosibirsk, 630090

T. Bul’bak

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: tomilen@igm.nsc.ru
Rússia, Novosibirsk, 630090

V. Sonin

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: tomilen@igm.nsc.ru
Rússia, Novosibirsk, 630090

A. Chepurov

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: tomilen@igm.nsc.ru
Rússia, Novosibirsk, 630090

N. Pokhilenko

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: tomilen@igm.nsc.ru
Rússia, Novosibirsk, 630090

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