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The Great Glen Crush-Belt

Published online by Cambridge University Press:  01 May 2009

V. A. Eyles  and
A. G. MacGregor
V. A. Eyles
Affiliation:
Geological Survey and Museum, Exhibition Road, London, S.W. 7
A. G. MacGregor
Affiliation:
Geological Survey and Museum, Exhibition Road, London, S.W. 7
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Abstract

This paper provides field and petrographic evidence believed by the authors to indicate that the Great Glen, over a lateral distance of some 40 miles between Fort William and Foyers, is flanked on the south-east by a broad crush-belt characterized by intense cataclasis and localized mylonitization. Most of the detailed evidence has not previously been published.

Type
Articles
Information
Geological Magazine , Volume 89 , Issue 6 , December 1952 , pp. 426 - 436
Copyright
Copyright © Cambridge University Press 1952

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References

REFERENCES

Bailey, E. B., 1934. West Highland Tectonics Loch Leven to Glen Roy. Quart. Journ. Geol. Soc., xc, 462–523.CrossRefGoogle Scholar
Kennedy, W. Q., 1946. The Great Glen Fault. Quart. Journ. Geol. Soc., cii, 41–72.CrossRefGoogle Scholar
Mould, D. D. C. P., 1946. The Geology of the Foyers “Granite” and the surrounding Country. Geol. Mag., lxxxiii, 249–265.Google Scholar
Shand, S. J., 1951. Mylonite, Slickensides, and the Great Glen Fault. Geol. Mag., lxxxviii, 423–8.Google Scholar