Hostname: page-component-78c5997874-xbtfd Total loading time: 0 Render date: 2024-11-18T04:29:38.563Z Has data issue: false hasContentIssue false
  • English
  • Français

The unit cell of talc

Published online by Cambridge University Press:  05 July 2018

M. Akizuki  and
J. Zussman
M. Akizuki
Affiliation:
Institute of Mineralogy, Petrology and Economic Geology, Tohoku University, Sendai, Japan
J. Zussman
Affiliation:
Department of Geology, University of Manchester, Manchester, England
Get access Rights & Permissions [Opens in a new window]

Summary

Six specimens of talc studied by the electron microscope lattice-imaging and diffraction techniques were found to have the triclinic one-layer (1 Tr) structure. Since no evidence of a monoclinic two-layered structure was found in any specimen it is concluded that the 1 Tr structure is the common one for talc, and it may, moreover, be the only one. Extremely fine polysynthetic twinning and single intrinsic stacking faults were found in talc.

Type
Research Article
Information
Mineralogical Magazine , Volume 42 , Issue 321 , March 1978 , pp. 107 - 110
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1978

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

Gruner, (J. W.), 1934, Z. Kristallogr. 88, 412-19.Google Scholar
Hendricks, (S. B.), 1938. Ibid. 99, 264-74.Google Scholar
Rayner, (J. S.) and Brown, (G.), 1973. Clays and Clay Miner. 21, 103-14.CrossRefGoogle Scholar
Ross, (M.), Smith, (W. L.), and Ashton, (W. H.), 1968. Am. Mineral. 53, 751-69.Google Scholar
Stemple, (I. S.) and Brindley, (G. W.), 1960. J. Am. Ceram. Soc. 43, 34-42.CrossRefGoogle Scholar
Zvyagin, (B. B.), 1967. Electron-diffraction analysis of clay mineral structures. (Transl. from the Russian), New York, Consultants Bureau.CrossRefGoogle Scholar