The pyrite-type high-pressure form of FeOOH

Masayuki Nishi (), Yasuhiro Kuwayama, Jun Tsuchiya () and Taku Tsuchiya
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Masayuki Nishi: Geodynamics Research Center, Ehime University
Yasuhiro Kuwayama: Geodynamics Research Center, Ehime University
Jun Tsuchiya: Geodynamics Research Center, Ehime University
Taku Tsuchiya: Geodynamics Research Center, Ehime University

Nature, 2017, vol. 547, issue 7662, 205-208

Abstract: The pyrite-type high-pressure form of FeOOH is predicted from first principles, and found experimentally to be stable under the conditions at the base of the mantle, with implications for transport of water within Earth’s deep interior.

Date: 2017
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DOI: 10.1038/nature22823

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