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An Exploratory Boring in the Lower Carboniferous of the Skipton Anticline

Published online by Cambridge University Press:  01 May 2009

R. G. S. Hudson
R. G. S. Hudson
Affiliation:
Department of Geology, The University, Leeds.
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Extract

Recent work on the succession and structure of the Skipton Anticline1 has proved strata about 6,000 feet thick. These beds are of Dinantian age ranging from γ to P2 and are in great contrast to the strata of the Askrigg massif, 8 miles to the north, where the Dinantian is of S1 to P2 age and is only 800 feet thick.

Type
Original Articles
Information
Geological Magazine , Volume 75 , Issue 11 , November 1938 , pp. 512 - 514
Copyright
Copyright © Cambridge University Press 1938

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References

1 Hudson, R. G. S., and Mitchell, G. H.,1937, Summ. Prog. Geol. Surv. for 1935, pt. ii, pp. 1–45.Google Scholar

2 Hudson, R. G. S., and Turner, J. S., 1933, Proc. Leeds Phil. Soc. Sci., Sect., ii, 467.Google Scholar

3 Paeckelmann, W., and Schindewolf, O. H., 1937, Compte rendu du deuxiéme Congrés pour l' avancement des études de Stratigraphie Carbonifére, Heerlen, 1935, ii, 703.Google Scholar

4 Jongmans, W. S., and Gothan, W., 1937, idem, i, 4.Google Scholar

5 Dixon, E. E. L., 1921, “Pembroke and Tenby,” Mem. Geol. Suru., Sheets 244 and 245, p. 48.Google Scholar

6 Vaughan, A., 1905, Quart. Journ. Geol. Soc., lxi, 251.Google Scholar

7 Sibly, T. F., and Reynolds, S. H., 1937, Quart. Journ. Geol. Soc., xciii, 23.CrossRefGoogle Scholar

8 Smyth, L. B., 1930, Proc. Roy. Irish Acad., xxxix, B, 523.Google Scholar