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Cross-bedding in the Millstone Grit of the central Pennines and its Significance

Published online by Cambridge University Press:  01 May 2009

M. D. Wright
M. D. Wright
Affiliation:
10 Elmfield Avenue, Manchester 22.
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Abstract

Most of the cross-bedding in the Central Pennine Millstone Grit occurs in the coarse sandstones and indicates that they are probably fluvial in origin. The cross-bedding often occurs within sheets of sandstone, and it is suggested that each sheet was deposited during one episode of flooding. Medium-grained arenaceous rocks show other varieties of cross-bedding that could have been formed on tidal flats, but this evidence is inconclusive.

Type
Articles
Information
Geological Magazine , Volume 101 , Issue 6 , 30 December 1964 , pp. 520 - 530
Copyright
Copyright © Cambridge University Press 1964

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References

REFERENCES

Allen, J. R. L., 1962. Asymmetrical ripple marks and the origin of cross-stratification. Nature, 194, 167–169.CrossRefGoogle Scholar
Allen, J. R. L., 1963. Structure of ripple marks. Nature, 198, 847–849.CrossRefGoogle Scholar
Häntzschel, W., 1936. Die Schichtungsformen rezenter Flachmeer-Ablagerungen im Jade-Gebiet. Senckenbergiana, 18, 316–356.Google Scholar
Knight, S. H., 1929. The Fountain and Casper formations of the Laramie Basin. Univ. Wyoming Publ. Sci., Geology 1, 1–82.Google Scholar
Richter, R., 1929. Gründung und Aufgaben der Forschungsstelle für Meeresgeologie “Senckenberg” in Wilhelmshaven. Natur und Museum, 59, 1–30.Google Scholar
Smith, A. L., 1909. Delta experiments. Bull. Amer. geogr. Soc., 41, 729–742.Google Scholar
Sorby, H. C., 1857. On the physical geography of the Tertiary estuary of the Isle of Wight. Edinburgh New Phil. Jour. (New Series), 5, 275–298.Google Scholar
Straaten, L. M. J. U. van, 1951. Texture and genesis of Dutch Wadden Sea sediments. Proc. 3rd Int. Cong. Sedimentology, 1951, p. 225–255.Google Scholar
Straaten, L. M. J. U. van, 1954. Sedimentology of Recent tidal flat deposits and the Psammites du Condroz (Devonian). Geol. en Mijnb. (New Ser.), 16, 25–47.Google Scholar
Thompson, W. O., 1937. Original structures of beaches, bars and dunes. Bull. geol. Soc. Amer., 48, 723–751.Google Scholar
Wright, M. D., 1959. The formation of cross-bedding by a meandering or braided stream. J. Sediment. Pet., 29, 610–615.Google Scholar