Pressure-induced magnetic transition and sound velocities of Fe3C: Implications for carbon in the Earth's inner core-Reference-Cited by-同舟云学术

Pressure-induced magnetic transition and sound velocities of Fe3C: Implications for carbon in the Earth's inner core

Published:2008-09-11 Issue:17 Volume:35 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Gao Lili,Chen Bin,Wang Jingyun,Alp Esen E.,Zhao Jiyong,Lerche Michael,Sturhahn Wolfgang,Scott Henry P.,Huang Fang,Ding Yang,Sinogeikin Stanislav V.,Lundstrom Craig C.,Bass Jay D.,Li Jie

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

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4. Ultrasonic study of the temperature and hydrostatic-pressure dependencies of the elastic properties of polycrystalline cementite;Dodd;Phys. Status Solidi A,2003

5. Magnetic instabilities in Fe3C cementite particles observed with Fe K-edge X-ray circular dichroism under pressure;Duman;Phys. Rev. Lett.,2005

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