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Infrared and Raman spectra of ZrSiO_4 experimentally shocked at high pressures

机译:实验高压冲击的ZrSiO_4的红外和拉曼光谱

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摘要

Zircon- and reidite-type ZrSiO_4 produced by shock recovery experiments at different pressures have been studied using infrared (IR) and Raman spectroscopy. The v_3 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 (I4_1/amd) to reidite (I4_1/a) is proven by the occurrence of additional IR and Raman bands. Although the SiO_4 groups in both zircon- and reidite-ZrSiO_4 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 ZrSiO_4 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.
机译:通过红外(IR)和拉曼光谱研究了在不同压力下通过冲击恢复实验生产的锆石和斑岩型ZrSiO_4。受到冲击的天然锆石中SiO_4基团的v_3振动显示出与辐射损坏的锆石中相似的光谱变化:频率降低,线宽增加。该观察结果可能暗示在受损和受冲击的锆石之间可能存在相似的缺陷晶体结构。冲击压力引起的结构相从锆石(I4_1 / amd)转变为菱铁矿(I4_1 / a)的现象已通过额外的IR和拉曼谱带的出现证明。尽管锆石-和锆石-ZrSiO_4中的SiO_4基团都被隔离,但更稠密的白钨矿在较低频率下会产生Si-O拉伸带,这表明键合强度减弱。 Reidite型ZrSiO_4的低温红外数据显示冷却对声子模的影响不明显,这表明Reidite对冷却诱导的压缩的结构响应较弱,并且其热膨胀很小。

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