Hostname: page-component-586b7cd67f-vdxz6 Total loading time: 0 Render date: 2024-11-30T20:31:16.479Z Has data issue: false hasContentIssue false

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*
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
*

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
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2009

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Bailey, S.W. (1980) Structures of layer silicates. Pp. 1124 in: Crystal Structures of Clay Minerals and their X-ray Identification (Brindley, G.W. and Brown, G., editors). Monograph 5, Mineralogical Society, London.Google Scholar
Bailey, S.W. (1984) Crystal chemistry of the true micas. Pp. 1360 in: Micas (Bailey, S.W., editor). Reviews in Mineralogy, 13, Mineralogical Society of America, Washington, D.C. Google Scholar
Bailey, S.W. (1988) Polytypism of 1:1 layer silicates. Pp. 1360 in: Hydrous Phyllosilicates (Exclusive of Micas) (Bailey, S.W., editor). Reviews in Mineralogy, 19, Mineralogical Society of America, Washington, D.C. Google Scholar
Guggenheim, S., Adams, J.M., Bain, D.C., Bergaya, F., Brigatti, M.F., Drits, V.A., Formoso, M.L.L., Galan, E., Kogure, T. and Stanjek, H. (2006) Summary of recommendations of nomenclature committees relevant to clay mineralogy: Report of the Association Internationale pour PEtude des Argiles (AIPEA) Nomenclature Committee for 2006. Clay Minerals, 41, 863878.Google Scholar
Kogure, T., Banno, Y. and Miyawaki, R. (2004) Interlayer structure in aspidolite, the Na analogue of phlogopite. European Journal of Mineralogy, 16, 891897.CrossRefGoogle Scholar
Kogure, T., Miyawaki, R. and Banno, Y. (2005) True structure of wonesite, an interlayer-deficient trioctahedral sodium mica. American Mineralogist, 90, 725731.Google Scholar
Kogure, T., Jige, M., Kameda, J., Yamagishi, A. and Kitagawa, R. (2006) Stacking structures in pyrophyllite revealed by high-resolution transmission electron microscopy (HRTEM). American Mineralogist, 91, 12931299.Google Scholar
Zvyagin, B.B., Mishchenko, K.S. and Soboleva, S.V. (1969) Structure of pyrophyllite and talc in relation to the polytypes of mica-type minerals. Soviet Physics-Crystallography, 13, 511515.Google Scholar