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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Abstract

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.

About the authors

A. A. Tomilenko

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Author for correspondence.
Email: tomilen@igm.nsc.ru
Russian Federation, Novosibirsk, 630090

E. I. Zhimulev

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: tomilen@igm.nsc.ru
Russian Federation, Novosibirsk, 630090

T. A. Bul’bak

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: tomilen@igm.nsc.ru
Russian Federation, Novosibirsk, 630090

V. M. Sonin

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: tomilen@igm.nsc.ru
Russian Federation, Novosibirsk, 630090

A. I. Chepurov

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: tomilen@igm.nsc.ru
Russian Federation, Novosibirsk, 630090

N. P. Pokhilenko

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: tomilen@igm.nsc.ru
Russian Federation, Novosibirsk, 630090

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