X-ray diffraction study of high pressure transition in InOOH

Asami Sano, Takehiko Yagi, Taku Okada, Hirotada Gotou, Eiji Ohtani, Jun Tsuchiya, Takumi Kikegawa

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15 Citations (Scopus)

Abstract

We performed high-pressure and high-temperature X-ray diffraction experiments on InOOH using laser heated diamond anvil cells. After heating at i300 K, pyrite-type InOOH was formed at 14 GPa and it was stable up to at least 30 GPa. Pyrite-type InOOH partially transformed back to distorted rutile-type InOOH after recovery. The lattice constant and unit-cell volume of pyrite-type InOOH were determined to be a0 = 5.3151(8) Å and V0 = 150.15 (7) Å3 at ambient conditions, respectively. The density difference between pyrite-type and distorted rutile-type InOOH was 5% at ambient condition.

Original languageEnglish
Pages (from-to)152-155
Number of pages4
JournalJournal of Mineralogical and Petrological Sciences
Volume103
Issue number2
DOIs
Publication statusPublished - 2008 Jun 30

Keywords

  • High pressure
  • InOOH
  • Pyrite-type structure

ASJC Scopus subject areas

  • Geophysics
  • Geology

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    Sano, A., Yagi, T., Okada, T., Gotou, H., Ohtani, E., Tsuchiya, J., & Kikegawa, T. (2008). X-ray diffraction study of high pressure transition in InOOH. Journal of Mineralogical and Petrological Sciences, 103(2), 152-155. https://doi.org/10.2465/jmps.071022m