Hostname: page-component-cd9895bd7-gxg78 Total loading time: 0 Render date: 2024-12-26T09:38:59.904Z Has data issue: false hasContentIssue false
  • English
  • Français

X-ray diffraction study of orientation of the micaceous minerals in slate

Published online by Cambridge University Press:  09 July 2018

Laila A. Fayed
Laila A. Fayed*
Affiliation:
Postgraduate School of Mining, University of Sheffield
Get access Rights & Permissions [Opens in a new window]

Abstract

An X-ray diffraction technique has been used to determine the orientation pattern of the (001) planes of 10 Å micaceous minerals in slate. The guiding principle of this technique is the direct measurement of the diffracted radiation from the pre-selected family of crystallographic planes as a function of the orientation of the specimen.

Results obtained indicated that the basal planes of these minerals are mostly oriented in a direction parallel to the cleavage planes and the possibility of another orientation was considered to be slight.

Type
Research Article
Information
Clay Minerals , Volume 6 , Issue 4 , December 1966 , pp. 333 - 340
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1966

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

Bates, T.F. (1947) Am. Miner. 30, 625.Google Scholar
Fayed, L.A. (1966) Ph.D. thesis, Sheffield University.Google Scholar
Gehien, K.V. (1960) Beitr. Miner. Petrogr. 7, 340.Google Scholar
Higgs, D.V., Friedman, M. & Gebhart, J.E. (1960) Mem. geol. Soc. Am. 79, 275.Google Scholar
Schulz, L.C. (1949a) J. appl. Phys. 20, 1030.Google Scholar
Schulz, L.C. (1949b) J. appl. Phys. 20, 1033.Google Scholar
Silverman, E.N. (1955) M.Sc. thesis. The Pennsylvania State University.Google Scholar
Silverman, E.N. & Bates, T.F. (1960) Am. Miner. 45, 60.Google Scholar