Refined Relationships between Chemical Composition of Dioctahedral Fine-Grained Mica Minerals and Their Infrared Spectra within the OH Stretching Region. Part I: Identification of the OH Stretching Bands
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[1] V. Drits,et al. Refined Relationships between Chemical Composition of Dioctahedral Fine-Grained Micaceous Minerals and Their Infrared Spectra Within the OH Stretching Region. Part II: The Main Factors Affecting OH Vibrations and Quantitative Analysis , 1997 .
[2] V. Drits,et al. Analysis of cation distribution in dioctahedral micaceous minerals on the basis of IR spectroscopy data , 1987, Clay Minerals.
[3] D. Eberl,et al. Sericite from the Silverton Caldera, Colorado; correlation among structure, composition, origin, and particle thickness , 1987 .
[4] V. Drits,et al. Interpretation of the IR spectra of celadonites and glauconites in the region of OH-stretching frequencies , 1986, Clay Minerals.
[5] G. Brindley,et al. Structural and IR relations among brucite-like divalent metal hydroxides , 1984 .
[6] B. Velde. Infrared spectra of synthetic micas in the series muscovite-MgAl celadonite , 1978 .
[7] V. Drits,et al. The Ferric Analogue of Pyrophyllite and Related Phases , 1979 .
[8] V. Farmer. The Layer Silicates , 1974 .
[9] S. Shimoda,et al. A FERRIC CELADONITE IN AMYGDALES OF DOLERITE AT TAIHEIZAN, AKITA PREFECTURE, JAPAN , 1973 .
[10] B. Saksena. Infra-red hydroxyl frequencies of muscovite, phlogopite and biotite micas in relation to their structures , 1964 .