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Some Discordant Fold Structures from the Dalradian of Craignish, Argyll, and Rosguill, Co. Donegal

Published online by Cambridge University Press:  01 May 2009

J. L. Knill  and
D. C. Knill
J. L. Knill
Affiliation:
Department of Geology, Imperial College, London S.W.7.
D. C. Knill
Affiliation:
Department of Geology, Imperial College, London S.W.7.
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Abstract

The paper describes minor fold structures, from the Dalradian of Scotland and Donegal which, following their formation, appear to have suffered partial rotation. These folds lie with their axial directions at an angle to the regional fold pattern.

Information

Type
Articles
Information
Geological Magazine , Volume 95 , Issue 6 , December 1958 , pp. 497 - 510
Copyright
Copyright © Cambridge University Press 1958

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References

REFERENCES

McCall, G. J. H., 1954. The Dalradian Geology of the Creeslough area, Co. Donegal. Quart. Journ. Geol. Soc., cx. 153–175.CrossRefGoogle Scholar
Peach, B. N., Kynaston, H., and Muff, H. B.., 1909. The Geology of the Seaboard of Mid-Argyll. Mem. Geol. Surv. Scotland, No. 36.Google Scholar