Hostname: page-component-848d4c4894-r5zm4 Total loading time: 0 Render date: 2024-06-30T06:06:52.118Z Has data issue: false hasContentIssue false
  • English
  • Français

Transparent packing models of layer-lattice silicates based on the observed structure of muscovite

Published online by Cambridge University Press:  14 March 2018

E. W. Radoslovich  and
J. B. Jones
E. W. Radoslovich
Affiliation:
Division of Soils, C.S.I.R.O., Adelaide, Australia
J. B. Jones
Affiliation:
Department of Geology, University of Adelaide, Australia
Get access

Abstract

A simple jig is described for the construction of a model of the muscovite structure in which the distorted hexagonal, i.e., ditrigonal, arrangement of the basal oxygens of the tetrahedra is accurately represented. The model is of the packing kind as opposed to the ball-and-spoke kind and demonstrates the advantages of this type of model, which would be more generally used if transparent plastic balls were available commercially.

Type
Research Article
Information
Clay Minerals Bulletin , Volume 4 , Issue 26 , December 1961 , pp. 318 - 322
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1961

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

Hatch, R. E., Comeforo, J. E., and Pace, N. A., 1952. Amer. Min., 37, 58.Google Scholar
Jackson, W. W., and West, J., 1930. Z. Kristallogr., 76, 211.CrossRefGoogle Scholar
Radoslovich, E. W., 1959. Nature, Lond., 183, 253.Google Scholar
Radoslovich, E. W., 1960. Acta Cryst., 13, 919.CrossRefGoogle Scholar
Radoslovich, E. W., 1961. Nature, Lond., 191, 67.Google Scholar