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Nomenclature for stacking in phyllosilicates: Report of the Association Internationale pour l'Etude des Argiles (AIPEA) Nomenclature Committee for 2008

Published online by Cambridge University Press:  09 July 2018

S. Guggenheim ,
J. M. Adams ,
F. Bergaya ,
M. F. Brigatti ,
V. A. Drits ,
M. L. L. Formoso ,
E. Galán ,
T. Kogure ,
H. Stanjek  and
J. W. Stucki
S. Guggenheim*
Affiliation:
Department of Earth and Environmental Sciences, University of Illinois at Chicago, 845 W. Taylor St., Chicago, Illinois 60607, USA
J. M. Adams
Affiliation:
(ex officio, Principal Editor, Clay Minerals), Department of Engineering, School of Engineering and Computer Science, University of Exeter, Harrison Building, North Park Road, Exeter EX44 QF, United Kingdom
F. Bergaya
Affiliation:
Centre de Recherche de la Matière Divisée, CNRS (National Center of Scientific Research)-University of Orléans, 1b Rue de la Férollerie, 45 071 Orléans Cedex 2, France
M. F. Brigatti
Affiliation:
Department of Earth Sciences, University of Modena, Largo S. Eufemia 19, I-41100, Modena, Italy
V. A. Drits
Affiliation:
Geological Institute of the Russian Academy of Science, 7 Pyzerskii Per, Moscow J-17 Russia
M. L. L. Formoso
Affiliation:
9500, Ave Bento Gonçalves, Campus do Vale, Instit. of Geosciences, University Federal do Rio Grande do Sul, Porto Alegre - RS - Brazil, CEP-91540-000
E. Galán
Affiliation:
Departmento de Cristalografía y Mineralogía, Facultad de Química, Universidad de Sevilla, 41071 Sevilla, Spain
T. Kogure
Affiliation:
Department of Earth and Planetary Science, Graduate School of Science, University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo, Japan
H. Stanjek
Affiliation:
Clay and Interface Mineralogy, RWTH Aachen University, Wuellnerstr. 2, D52056 Aachen, Germany
J. W. Stucki
Affiliation:
(ex officio, Editor-in-Chief, Clays and Clay Minerals), Department of Natural Resources and Environmental Sciences, 1102 S. Goodwin Ave., University of Illinois, Urbana, Illinois, 61801, USA
*
*E-mail: xtal@uic.edu
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Extract

Kogure and co-workers have published several papers reporting the stacking structures of various 2:1 layer phyllosilicates (e.g. aspidolite, Kogure et al. (2004); wonesite, Kogure et al. (2005); pyrophyllite, Kogure et al. (2006)), mainly by using high-resolution transmission electron microscopy (HR-TEM). However, there is ambiguity in wording that refers to the lateral displacement between two tetrahedral sheets across the interlayer regions. Zvyagin et al. (1969) used the symbol “τ” for this displacement, which describes the structures of pyrophyllite and talc, but no universally accepted wording was used for other 2:1 phyllosilicates or 1:1 phyllosilicates.

Type
Research Article
Information
Clay Minerals , Volume 44 , Issue 1 , March 2009 , pp. 157 - 159
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2009

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References

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