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Kink-bands in Lower Carboniferous Slates of Rush, Co. Dublin

Published online by Cambridge University Press:  01 May 2009

Abstract

Unusual single kink-band sets in calcareous slates are described and their mechanism of formation discussed. Regional inferences are drawn concerning Armorican strike-slip movements.

Type
Articles
Copyright
Copyright © Cambridge University Press 1966

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References

REFERENCES

Anderson, T. B., 1964. Kink bands and related geological structures. Nature, 202, No. 2429, 272–4.CrossRefGoogle Scholar
Dewey, J. F., 1965. On the nature and origin of kink-bands. Tectonophysics. (In press).CrossRefGoogle Scholar
Flinn, D., 1952. A tectonic analysis of the Muness Phyllite block of Unst and Uyea, Shetland. Geol. Mag., 89, 263272.CrossRefGoogle Scholar
Gill, W. D., 1962. The Variscan fold belt in Ireland. In Some aspects of the Variscan fold belt. Manchester University Press.Google Scholar
Kienow, S., 1934. Die innere Tektonik des Unterdevons zwischen Rhein, Mosel und Nahe. Jb. preuss. geol. Landesanst, 54, 5895.Google Scholar
Matley, C. A., 1906. The Carboniferous rocks at Rush (Co. Dublin). Quart. J. geol. Soc. Lond., 62, 275322.CrossRefGoogle Scholar
Smyth, L. B., 1915. On the faunal zones of the Rush-Skerries Carboniferous section, Co. Dublin. Sci. Proc. R. Dublin Soc., 14, 535562.Google Scholar
Ramsay, J. G., 1962. The geometry of conjugate fold systems. Geol. Mag., 99, 7593.CrossRefGoogle Scholar