Raman spectroscopic study of K-lingunite at various pressures and temperatures

被引:0
作者
Lin-gun Liu
C.-C. Lin
Y. J. Yung
T. P. Mernagh
T. Irifune
机构
[1] Institute of Earth Sciences,Geodynamics Research Center
[2] Academia Sinica,Department of Earth Sciences
[3] Geoscience Australia,undefined
[4] Ehime University,undefined
[5] The University of Hong Kong,undefined
来源
Physics and Chemistry of Minerals | 2009年 / 36卷
关键词
K-lingunite; Raman spectroscopy; High pressure; High temperature;
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学科分类号
摘要
K-lingunite is a high-pressure modification of K-feldspar that possesses the tetragonal hollandite structure. Variations of the Raman spectra of K-lingunite were studied up to ~31.5 GPa at room temperature, and in the range 79–823 K at atmospheric pressure. The Raman frequencies of all bands were observed to increase with increasing pressure, and decrease with increasing temperature for K-lingunite. This behavior is in line with those observed for most of other materials. New sharp Raman bands appear at pressures greater than 13–15 GPa, suggesting a phase transition in K-lingunite with increasing pressure. The transition is reversible when pressure was released. The appearance of these new Raman bands may correspond to the phase transition revealed earlier at around 20 GPa by X-ray diffraction studies. Instead of transforming back to its stable minerals, such as orthoclase, microcline or sanidine, K-lingunite became amorphous in the temperature range 803–823 K at atmospheric pressure.
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页码:143 / 149
页数:6
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