A Raman spectroscopic study of phengite under high pressure
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P578.959 O433

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    Abstract:

    Within the diamond anvil cell, the Raman spectroscopic study of phengite was developed at room temperature and under various pressures from 1 atmp to 20 GPa. The authors analyzed the correlation of the modes 266, 708 and 3618 cm-1 with the variation of pressure. The mode of 708 cm-1 increases linearly with the increase of pressure, i.e., y (Raman shift, cm-1)=0.5238x (pressure, GPa) +712.31, and R2 (correlation coefficient)=0.9656, and the mode disappears at 4.7 GPa as a result of substituting Si for Al. The mode of OH- band and the intensity decrease linearly with the increase of pressure, i.e., y=-0.3402 x+3617.8 and R2=0.9662, and the mode disappears at 18 GPa, which is assumed to be the maximum pressure for the dehydration of phengite at room temperature.

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曹淑慧 张立飞 孙樯 郑海飞 崔光来,2006,高压下多硅白云母的拉曼光谱学研究[J].岩石矿物学杂志,25(1):71~76. CAO Shu-hui, ZHANG Li-fei, SUN Qiang, ZHENG Hai-fei, CUI Guang-lai,2006,A Raman spectroscopic study of phengite under high pressure[J]. Acta Petrologica et Mineralogica,25(1):71~76.

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  • Received:April 01,2005
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