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 language | English |
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Pages (from-to) | 801-811 |
Number of pages | 11 |
Journal | Mineralogical Magazine |
Volume | 68 |
Issue number | 5 |
DOIs | |
Publication status | Published - Oct 2004 |
Externally published | Yes |
ASJC Scopus Subject Areas
- Geochemistry and Petrology
Keywords
- High pressure
- Infrared spectroscopy
- Metamictization
- Phase transition
- Raman spectroscopy
- Reidite
- Scheelite structure
- Zircon
- ZrSiO