Physics and Chemistry of Minerals

, Volume 19, Issue 6, pp 357–360 | Cite as

Phase E: A high pressure hydrous silicate with unique crystal chemistry

  • Y. Kudoh
  • L. W. Finger
  • R. M. Hazen
  • C. T. Prewitt
  • M. Kanzaki
  • D. R. Veblen
Article

Abstract

The unique cation-disordered crystal structures of two samples of phase E, a non-stoichiometric, hydrous silicate synthesized in a uniaxial, split-sphere, multi-anvil apparatus at conditions above 13 GPa and 1000° C, have been solved and refined in space group \(\bar 3\). The compositions and unit cells for the two materials, assuming six oxygens per cell, are Mg2.08Si1.16H3.20O6, a=2.9701(1) Å, c=13.882(1) Å V = 106.05(4) Å3 for sample 1, and Mg2.17Si1.01H3.62O6, a=2.9853(6) Å, c=13.9482(7) Å, V= 107.65(4) Å3 for sample 2. The structure contains layers with many features of brucite-type units, with the layers stacked in a rhombohedral arrangement. The layers are cross linked by silicon in tetrahedral coordination and magnesium in octahedral coordination, as well as hydrogen bonds. Interlay er octahedra share edges with intralayer octahedra. Interlayer tetrahedra would share faces with intralayer octahedra. To avoid this situation, there are vacancies within the layers. There is, however, no long-range order in the occupation of these sites, as indicated by the lack of a superstructure. Selected-area electron diffraction patterns show walls of diffuse intensity similar in geometry and magnitude to those observed in short-range-ordered alloys and Hågg phases. Phase E thus appears to represent a new class of disordered silicates, which may be thermodynamically metastable.

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Copyright information

© Springer-Verlag 1993

Authors and Affiliations

  • Y. Kudoh
    • 1
  • L. W. Finger
    • 1
  • R. M. Hazen
    • 1
  • C. T. Prewitt
    • 1
  • M. Kanzaki
    • 2
    • 4
  • D. R. Veblen
    • 3
  1. 1.Geophysical LaboratoryCarnegie Institution of WashingtonUSA
  2. 2.Department of GeologyUniversity of AlbertaEdmontonCanada
  3. 3.Department of Earth and Planetary SciencesJohns Hopkins UniversityBaltimoreUSA
  4. 4.Department of Inorganic Materials, Faculty of EngineeringTokyo Institute of TechnologyTokyoJapan
  5. 5.Institute of Mineralogy, Petrology and Economic Geology, Faculty of ScienceTohuku UniversitySendaiJapan

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