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Structure-Composition Relationships in Trioctahedral Chlorites: A Vibrational Spectroscopy Study

Published online by Cambridge University Press:  02 April 2024

A. C. Prieto
Affiliation:
Departamento de Fisica de la Materia Condensada, Cristalografia y Mineralogia, Universidad de Valladolid, 47011, Valladolid, Spain
J. Dubessy
Affiliation:
CREGU and GS CNRS-CREGU, BP 23, 54501, Vandoeuvre les Nancy Cedex, France
M. Cathelineau
Affiliation:
CREGU and GS CNRS-CREGU, BP 23, 54501, Vandoeuvre les Nancy Cedex, France
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Abstract

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Raman and Fourier-transformed infrared spectra of natural trioctahedral chlorites of polytype IIb were obtained for a series of samples characterized by distinct Fe/(Fe + Mg) and Si/Al ratios ranging, respectively, from 0.04 to 0.94 and from 5.18 to 1.86. All samples were characterized by X-ray powder diffraction, and quantitative electron microprobe analysis. In the 3683-3610-cm−1 spectral range, the wave number of the OH-stretching band from the 2:1 layer (band I) decreased with an increase of iron content at constant Al(IV) content. The more intense bands II and III at about 3600 cm−1 and 3500 cm−1, were assigned to hydroxyl groups involved in hydrogen bonds: (SiSi)O... HO, with the hydrogen bonds being roughly perpendicular to the basal plane, and (SiAl)O... HO, respectively. At higher tetrahedral Al and octahedral Fe contents, spectra exhibited OH-bands II and III, respectively, at a lower frequency. Band III intensity increased and band II was enlarged for chlorites displaying higher Al(IV) contents.

In the 1300–1350-cm−1 spectral range, most infrared spectra displayed intense bands at 1090, 1050, 990, and 960 cm−1, which were assigned to T-O stretching of symmetry species Al and E1. The second type of bands observed both in Raman and infrared spectra were at about 650–800 cm−1; they were assigned to OH vibrations and were strongly dependent on the composition of the interlayer octahedral sheet, especially on the Fe content.

Type
Research Article
Copyright
Copyright © 1991, The Clay Minerals Society

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