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引用次数: 1
摘要
对一组x = 0-5的合成角闪石Na(NaCa)(Mg5-xCox)Si8O22(OH)2的拉曼光谱进行了记录,这些角闪石先前已经用Rietveld结构细化和红外光谱在主OH-拉伸区进行了表征。由O-H拉伸拉曼峰强度得到的化学成分与标称成分一致,也与先前通过Rietveld结构精化和红外光谱测定的化学成分一致。从Leissner et al.(2015)和Waeselmann et al.(2019)的工作开始,已经对低波数区域(50-1200 cm-1)的拉曼光谱进行了详细的峰分配,以及Ivanov et al.(2018)给出的钾镁铝铝石结构中所有阳离子-阴离子对的模拟部分拉曼光谱。大多数拉曼峰表现出单模行为,并随着Co在角闪洞中的增加而向低波数偏移。
Raman and FTIR Spectroscopy of Synthetic Amphiboles: II. Divalent (Mg,Co) Substitutions at the Octahedrally Coordinated Sites
Raman spectra were recorded for a set of synthetic amphiboles, Na(NaCa)(Mg5–xCox)Si8O22(OH)2 with x = 0–5, that have been previously characterized by Rietveld structure refinement and infrared spectroscopy in the principal OH-stretching region. The chemical compositions derived from the intensities of the O-H stretching Raman peaks are in accord with the nominal compositions, as well as with the compositions previously determined by both Rietveld structure refinement and infrared spectroscopy. Detailed peak assignments have been made of the Raman spectra in the low-wavenumber region (50–1200 cm–1) starting from the work of Leissner et al. (2015) and Waeselmann et al. (2019) and the simulated partial Raman spectra for all the cation-anion pairs in the structure of potassic-magnesio-arfvedsonite given by Ivanov et al. (2018). Most Raman peaks exhibit one-mode behavior and shift toward lower wavenumbers for increasing Co in the amphibole.
期刊介绍:
Since 1962, The Canadian Mineralogist has published papers dealing with all aspects of mineralogy, crystallography, petrology, economic geology, geochemistry, and applied mineralogy.