Hostname: page-component-cd9895bd7-hc48f Total loading time: 0 Render date: 2024-12-23T06:22:05.140Z Has data issue: false hasContentIssue false

Structural Transformations of Interstratified Illite-Smectites from Dolná Ves Hydrothermal Deposits: Dynamics and Mechanisms

Published online by Cambridge University Press:  28 February 2024

V. A. Drits
Affiliation:
Geological Institute, Academy of Sciences, Moscow, Russia
A. L. Salyn
Affiliation:
Geological Institute, Academy of Sciences, Moscow, Russia
V. Šucha
Affiliation:
Geological Institute, Academy of Sciences, Moscow, Russia Comenius University, Bratislava, Slovakia
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Structural transformations of illite-smectite samples of hydrothermal genesis with increasing contents of illite layers were studied by X-ray powder diffraction. The samples were K-saturated and subjected to wetting and drying cycles to increase three-dimensional structural ordering. Diffraction profiles were analyzed with the help of a specially devised computer program based on the approximation of individual diffraction reflections by “bell-shaped” functions, with minimization of the differences between experimental and simulated profiles. The data indicate that the transformations of these illite-smectite samples were accompanied not only by variations in the proportion of illite and smectite layers and in the pattern of their alternation, but also by a change in structure within 2:1 layers.

Type
Research Article
Copyright
Copyright © 1996, The Clay Minerals Society

References

Drits, V.A.. 1987. Mixed-layer minerals: Diffraction methods and structural features. Proc. Intern. Clay Conf. Denver, 1985. Schultz LG, van Olphen H, Mumpton FA, editors. Bloomington (Ind.): Clay Miner. Soc. 3345.Google Scholar
Drits, V.A. and Kossovskaya, A.G.. 1991. Clay minerals: smectites and mixed-layer formations. Moscow: Nauka. 212p. (in Russian).Google Scholar
Drits, V.A., Plançon, A., Sakharov, B.A., Besson, G., Tsipursky, S.I. and Tchoubar, C.. 1984. Diffraction effects calculated for structural models of K-saturated montmorillonite containing different types of defects. Clay Miner 19: 541562.Google Scholar
Drits, V.A. and Sakharov, B.A.. 1976. X-ray diffraction structure analysis of mixed-layer minerals. Moscow: Nauka. 252p. (in Russian).Google Scholar
Drits, V.A., Weber, F., Salyn, A.L. and Tsipursky, S.. 1993. X-ray identification of one-layer illite varieties: application to the study of illites around uranium deposits. Clays & Clay Miner 41: 389398.CrossRefGoogle Scholar
Eberl, D.D.. 1993. Three zones for illite formation during burial diagenesis and metamorphism. Clays & Clay Miner 41: 2637.CrossRefGoogle Scholar
McCarty, D.K. and Reynolds, R.C.. 1995. Rotationally disordered illite/smectite. Clays & Clay Miner 43: 271284.CrossRefGoogle Scholar
Nadeau, P.H.. 1985. The physical dimensions of fundamental clay particles. Clay Miner 20: 499514.CrossRefGoogle Scholar
Nadeau, P.H., Wilson, M.J., McHardy, W.J. and Tait, J.M.. 1984. Interstratified clay as fundamental particles. Science 225: 923925.CrossRefGoogle Scholar
Nadeau, P.H., Wilson, M.J., McHardy, W.J. and Tait, J.M.. 1985. The conversion of smectite to illite during diagenesis: evidence from some illitic clays from bentonites and sandstones. Mineralogical Magazine 49: 393400.CrossRefGoogle Scholar
Peacor, D.R.. 1992. Diagenesis and low-grade metamorphism of shales and slates. In: Buseck, P.R., editor. Minerals and reactions at the atomic scale: transmission Electron Microscopy. Reviews in Mineralogy. Washington: Mineralogical Society of America 27: 335380.CrossRefGoogle Scholar
Reynolds, R.C.. 1980. Interstratified clay minerals. In: Brindley, G.W., Brown, G., editors. Crystal structures of clay minerals and their X-ray identification. London: Mineralogical Society. 249303.CrossRefGoogle Scholar
Reynolds, R.C.. 1993. Three-dimensional X-ray powder diffraction from disordered illite: simulation and interpretation of the diffraction patterns. In: Reynolds, R.C., Walker, J.R., editors. Computer applications to X-ray powder diffraction analysis of clay minerals. CMS workshop lectures, 5. Boulder: Clay Miner Soc of Am. 4378.Google Scholar
Salyn, A.L.. 1988. X-ray diffraction quantitative phase analysis of mixture of polytype or polymorph modifications. PhD Thesis, Moscow, Moscow University (in Russian).Google Scholar
Šucha, V., Kraus, I., Mosser, C.h., Hroncova, Z. and Siranova, V.. 1992. Mixed-layer illite/smectite from the Dovna Ves hydrothermal deposit, the Western Carpathians Kremnica MTS. Bratislava: Geologia Carpathica, Clays, series 1. 1: 1321.Google Scholar
Środoń, J. and Eberl, D.D.. 1984. Illites. In: Baily, S.W., editor. Micas. Reviews in Mineralogy. Mineral Soc Am 13: 495544.Google Scholar
Środoń, J., Elsass, F., McHardy, W.J. and Morgan, D.J.. 1992. Chemistry of illite-smectite inferred from TEM measurements of fundamental particles. Clay Miner 27: 137158.CrossRefGoogle Scholar
Tsipursky, S.I. and Drits, V.A.. 1984. The distribution of octahedral cations in the 2: 1 layers of dioctahedral smectites studied by oblique texture electron diffraction. Clay Miner 19: 177192.CrossRefGoogle Scholar