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Flow-Markings and Lode-Casts

Published online by Cambridge University Press:  01 May 2009

Ph. H. Kuenen and
J. E. Prentice
Ph. H. Kuenen
Affiliation:
Geological Institute, Melkweg 1, Groningen, Holland.
J. E. Prentice
Affiliation:
University of London, King's College, Strand, W.C. 2.
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Information

Type
Correspondence
Information
Geological Magazine , Volume 94 , Issue 2 , April 1957, pp. 173 - 174
Copyright
Copyright © Cambridge University Press 1957

References

REFERENCES

Dzulynski, St., and Radomski, A., 1955. Origin of groove casts in the light of turbidity currents hypothesis. Acta Geol. Polonica, v, 1955, 47–66.Google Scholar
Emery, K. O., 1950. Contorted Pleistocene strata at Newport Beach, California. Journ. Sed. Petr., xx, 111–15.Google Scholar
PhKuenen, H., 1953. Significant features of graded bedding. Bull. Amer. Ass. Petr. Geol., xxxvii, 1044–1066.Google Scholar
Macar, P., and Antun, P., 1950. Pseudo-nodules et glissement sous-aquatique dans l'Emsien inférieur de l'Oesling. Ann. Soc. Géol. Belg., lxxiii, B 121–150.Google Scholar
Prentice, J. E., 1956. The interpretation of flow-markings and load-casts. Geol. Mag., xciii, 393–400.CrossRefGoogle Scholar
Shrock, R. R., 1948. Sequence in layered rocks. New York.Google Scholar
Walton, E. K., 1956. Limitations of graded bedding: and alternative criteria of upward sequence in the rocks of the Southern Uplands. Trans. Edin. Geol. Soc., xvi, part iii, 262–271.CrossRefGoogle Scholar