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XX.—Ordovician Submarine Disturbances in the Girvan District

Published online by Cambridge University Press:  06 July 2012

S. M. K. Henderson
S. M. K. Henderson
Affiliation:
Geology Department, University of Glasgow.
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Extract

Investigations have been made into the conditions of sedimentation of the Ordovician rocks of the Girvan district, with special attention to a series of greywackes, the Ardwell Beds, which are remarkable for frequent intraformational disturbances and unconformities.

In presenting the evidence it is proposed to follow the stratigraphical classification of Peach and Horne (1899), who, after careful consideration, adopted Lapworth's (1882) succession, except for a few minor alterations. These authors pointed out that the Llandeilo rocks north of the River Stinchar consist of Kirkland Conglomerate, Stinchar Limestone Group, and Benan Conglomerate, while south of the river they are represented by Tappins Greywackes and Glen App Conglomerate (see table p. 488).

Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 58 , Issue 2 , 1935 , pp. 487 - 509
Copyright
Copyright © Royal Society of Edinburgh 1935

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References

References to Literature

Bailey, E. B., 1930. “New Light on Sedimentation and Tectonics,” Geol. Mag., vol. lxvii, p. 77.CrossRefGoogle Scholar
Bailey, E. B., Collet, L. W., and Field, R. M., 1928. “Palæozoic Landslips near Quebec City,” Journ. Geol., vol. xxxvi, No. 7, p. 577.CrossRefGoogle Scholar
Bailey, E. B., and Weir, J., 1932. “Submarine Faulting in Kimmeridgian Times: East Sutherland,” Trans. Roy. Soc. Edin., vol. lvii, pt. ii, p. 429.Google Scholar
Goodchild, J. G., 1901. “Canty Bay and the Bass,” Proc. Berwickshire Nat. Club, vol. xviii, pt. ii, app. I, p. 41.Google Scholar
Hadding, A., 1931. “On Subaqueous Slides,” Geol. Fören. Stockh. Förh., vol. liii, p. 377.CrossRefGoogle Scholar
Hahn, F. F., 1913. “Untermeerische Gleitung bei Trenton Falls,” Neues. Jahr. Min., Beil. Bd. xxxvi, p. 1.Google Scholar
Henderson, S. M. K., 1933. In “Summer Field Meeting, 1932; Girvan-Ballantrae,” Proc. Geol. Assoc., vol. lxiv, pt. i, pp. 57–86.Google Scholar
Lapworth, C., 1882. “The Girvan Succession,” Quart. Journ. Geol. Soc., vol. xxxviii, p. 537.CrossRefGoogle Scholar
Miller, W. J., 1922. “Intraformational Corrugated Rocks,” Journ. Geol., vol. xxx, p. 587.CrossRefGoogle Scholar
Norton, W. H., 1917. “Studies for Students—A Classification of Breccias,” Journ. Geol., vol. xxv, pp. 182–185.Google Scholar
Park, J., 1914. A Textbook of Geology, p. 22.Google Scholar
Peach, B. N., and Horne, J., 1899. “The Silurian Rocks of Britain,” vol. i (Scotland), Mem. Geol. Survey.Google Scholar
Richardson, W. A., 1921. “The Relative Age of Concretions,” Geol. Mag., vol. lviii, p. 114.CrossRefGoogle Scholar
Sorby, R. H., 1908. “On Application of Quantitative Methods to the Study of Rocks,” Quart. Journ. Geol. Soc., vol. lxiv, p. 197.Google Scholar
Twenhofel, W. H., 1932. Treatise on Sedimentation, 2nd ed., 1932.Google Scholar
Wills, L. J., 1929. The Physiographical Evolution of Britain, pp. 256–271.Google Scholar