Synthesis of New Polytypic Modifications of Fe7C3 at 5.5 GPa


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The results of experimental synthesis of carbide Fe7C3 at 5.5 GPa are presented. It is found that carbide Fe3C and several polytypes of carbide Fe7C3 are formed along with diamond during cooling of the system. It is considered that the Fe7C3 phase is a component of the Earth’s inner core. Our results indicate that polytypic carbide modifications could have been formed under natural conditions at relatively low pressures during differentiation of the Earth.

作者简介

A. Chepurov

Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences

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Email: chepurov@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090

S. Gromilov

Nikolaev Institute of Inorganic Chemistry, Siberian Branch, Russian Academy of Sciences; Novosibirsk National Research State University

Email: chepurov@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090; Novosibirsk, 630090

V. Sonin

Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences

Email: chepurov@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090

E. Zhimulev

Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences

Email: chepurov@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090

A. Sukhikh

Nikolaev Institute of Inorganic Chemistry, Siberian Branch, Russian Academy of Sciences; Novosibirsk National Research State University

Email: chepurov@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090; Novosibirsk, 630090

A. Chepurov

Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences

Email: chepurov@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090

N. Sobolev

Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences; Novosibirsk National Research State University

Email: chepurov@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090; Novosibirsk, 630090

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