Infrared and Raman spectra of ZrSiO4 experimentally shocked at high pressures

A. Gucsik, M. Zhang*, C. Koeberl, E. K.H. Salje, S. A.T. Redfern, J. M. Pruneda

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

66 Citations (Scopus)

Abstract

Zirco- and reidite-type ZrSiO4 produced by shock recovery experiments at different pressures have been studied using infrared (IR) and Raman spectroscopy. The v3 vibration of the SiO 4 group in shocked natural zircon shows a spectral change similar to that seen in radiation-damaged zircon: a decrease in frequency and increase in linewidth. The observation could imply a possible similar defective crystal structure between the damaged and shocked zircon. The shock-pressure-induced structural phase transition from zircon (I41/amd) to reidite (I41/a) is proven by the occurrence of additional IR and Raman bands. Although the SiO 4 group in both zircon- and reidite-ZrSiO4 are isolated, the more condensed scheelite gives rise to Si-O stretching bands at lower frequencies, suggesting a weakening of the bond strength. Low-temperature IR data of the reidite-type ZrSiO4 show an insignificant effect of cooling on the phonon modes, suggesting that the structural response of reidite to cooling-induced compression is weak and its thermal expansion is very small.

Original languageEnglish
Pages (from-to)801-811
Number of pages11
JournalMineralogical Magazine
Volume68
Issue number5
DOIs
Publication statusPublished - Oct 2004
Externally publishedYes

ASJC Scopus Subject Areas

  • Geochemistry and Petrology

Keywords

  • High pressure
  • Infrared spectroscopy
  • Metamictization
  • Phase transition
  • Raman spectroscopy
  • Reidite
  • Scheelite structure
  • Zircon
  • ZrSiO

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