Ultrahigh-pressure disordered eight-coordinated phase of Mg2GeO4: Analogue for super-Earth mantles

Rajkrishna Dutta, Sally June Tracy, R. E. Cohen, Francesca Miozzi, Kai Luo, Jing Yang, Pamela C. Burnley, Dean Smith, Yue Meng, Stella Chariton, Vitali B. Prakapenka, Thomas S. Duffy

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Mg2GeO4 is important as an analog for the ultrahigh-pressure behavior of Mg2SiO4, a major component of planetary interiors. In this study, we have investigated magnesium germanate to 275 GPa and over 2,000 K using a laser-heated diamond anvil cell combined with in situ synchrotron X-ray diffraction and density functional theory (DFT) computations. The experimental results are consistent with the formation of a phase with disordered Mg and Ge, in which germanium adopts eightfold coordination with oxygen: the cubic, Th3P4-type structure. DFT computations suggest partial Mg-Ge order, resulting in a tetragonal I42 - d structure indistinguishable from I43 - d Th3P4 in our experiments. If applicable to silicates, the formation of this highly coordinated and intrinsically disordered phase may have important implications for the interior mineralogy of large, rocky extrasolar planets.

Original languageEnglish (US)
Article numbere2114424119
JournalProceedings of the National Academy of Sciences of the United States of America
Issue number8
StatePublished - Feb 22 2022

All Science Journal Classification (ASJC) codes

  • General


  • Order-disorder transition
  • Post-postperovskite
  • Super-Earth mineralogy


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