Structural complexity of simple Fe2O3 at high pressures and temperatures-Reference-Cited by-同舟云学术

Structural complexity of simple Fe2O3 at high pressures and temperatures

Published:2016-02-11 Issue:1 Volume:7 Page:
ISSN:2041-1723
Container-title:Nature Communications
language:en
Short-container-title:Nat Commun

Author:

Bykova E.,Dubrovinsky L.,Dubrovinskaia N.,Bykov M.^ORCID,McCammon C.^ORCID,Ovsyannikov S. V.,Liermann H. -P.,Kupenko I.,Chumakov A. I.,Rüffer R.,Hanfland M.,Prakapenka V.

Publisher

Springer Science and Business Media LLC

Subject

General Physics and Astronomy,General Biochemistry, Genetics and Molecular Biology,General Chemistry

Link

http://www.nature.com/articles/ncomms10661.pdf

Reference42 articles.

1. Shim, S.-H. et al. Electronic and magnetic structurses of the postperovskite-type Fe2O3 and implications for planetary magnetic records and deep interiors. Proc. Natl Acad. Sci. USA 106, 5508–5512 (2009).

2. Dobson, D. P. & Brodholt, J. P. Subducted banded iron formations as a source of ultralow-velocity zones at the core-mantle boundary. Nature 434, 371–374 (2005).

3. Tuček, J. et al. Zeta-Fe2O3–A new stable polymorph in iron(III) oxide family. Sci. Rep. 5, 15091 (2015).

4. Olsen, J. S., Cousins, C. S. G., Gerward, L., Jhans, H. & Sheldon, B. J. A study of the crystal structure of Fe2O3 in the pressure range up to 65 GPa using synchrotron radiation. Phys. Scr. 43, 327–330 (1991).

5. Pasternak, M. et al. Breakdown of the Mott-Hubbard state in Fe2O3: A first-order insulator-metaltransition with collapse of magnetism at 50 GPa. Phys. Rev. Lett. 82, 4663–4666 (1999).

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