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The Formation of the Hydraulic Limestones of the Lower Lias

Published online by Cambridge University Press:  01 May 2009

P. E. Kent
P. E. Kent
Affiliation:
University College, Nottingham.
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Extract

AS a result of a study of the Liassic limestones of the Dorset coast, Dr. W. A. Richardson (1923) concluded that both the limestone bands and the nodules were of secondary origin, and largely displaced the associated marls and shales. Observations made during a study of the Hydraulic Limestone Series (pre-planorbis-johnstoni subzones) in south Nottinghamshire lend support to the hypothesis of concretionary origin, but do not accord with certain other of Dr. Richardson's suggestions.

Type
Original Articles
Information
Geological Magazine , Volume 73 , Issue 10 , October 1936 , pp. 476 - 478
Copyright
Copyright © Cambridge University Press 1936

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References

REFERENCE

Richardson, W. A., 1923. “On the Petrology of the Shales-with- ‘Beef’,” Quart. Journ. Geol. Soc., lxxix, part 1, pp. 88–98.CrossRefGoogle Scholar