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Interpretation of the IR spectra of celadonites and glauconites in the region of OH-stretching frequencies

Published online by Cambridge University Press:  09 July 2018

M. V. Slonimskaya ,
G. Besson ,
L. G. Dainyak ,
C. Tchoubar  and
V. A. Drits
M. V. Slonimskaya
Affiliation:
Geological Institute of Geology, Pijevsky Street 7, MoscowUSSR
G. Besson
Affiliation:
Laboratoire de Cristallographie (UA 810), Université d'Orléans, Rue de Chartres, BP 6057, 45067 Orléans Cédex 2, France
L. G. Dainyak
Affiliation:
Geological Institute of Geology, Pijevsky Street 7, MoscowUSSR
C. Tchoubar
Affiliation:
Laboratoire de Cristallographie (UA 810), Université d'Orléans, Rue de Chartres, BP 6057, 45067 Orléans Cédex 2, France
V. A. Drits
Affiliation:
Geological Institute of Geology, Pijevsky Street 7, MoscowUSSR
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Abstract

A method is given for quantitative analysis of IR spectra of dioctahedral micas in the OH-stretching region, which involves spectral decomposition and correlation of octahedral cation contents with integrated optical densities of the corresponding bands. It provides a basis for the study of order-disorder in these minerals and has allowed revision of the crystallochemical formulae of some glauconites and celadonites.

Type
Research Article
Information
Clay Minerals , Volume 21 , Issue 3 , September 1986 , pp. 377 - 388
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1986

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