4.3 Article

Infrared and Raman spectra of ZrSiO4 experimentally shocked at high pressures

期刊

MINERALOGICAL MAGAZINE
卷 68, 期 5, 页码 801-811

出版社

MINERALOGICAL SOC
DOI: 10.1180/0026461046850220

关键词

ZrSiO4; zircon; reidite; scheelite structure; high pressure; phase transition; infrared spectroscopy; Raman spectroscopy; metamictization

向作者/读者索取更多资源

Zircon- and reidite-type ZrSiO4 produced by shock recovery experiments at different pressures have been studied using infrared (IR) and Raman spectroscopy. The nu(3) vibration of the SiO4 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 (I4(1)/amd) to reidite (I4(1)/a) is proven by the occurrence of additional IR and Raman bands. Although the SiO4 groups 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.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.3
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据