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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
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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

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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