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The Origin of the Supposed Tufa Bands in Carboniferous Reef Limestones

Published online by Cambridge University Press:  01 May 2009

W. W. Black
W. W. Black
Affiliation:
Geology Department, University of Nottingham
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Abstract

Thin bands of fibrous calcite occur in the Carboniferous reef limestones of northern England and have been regarded as bands of primary tufa within a marine limestone series. A study of these fibrous bands has been carried out and the results show conclusively that they are in fact secondary recrystallization structures.

Type
Articles
Information
Geological Magazine , Volume 89 , Issue 3 , June 1952 , pp. 195 - 200
Copyright
Copyright © Cambridge University Press 1952

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References

REFERENCES

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Parkinson, D., 1950. The stratigraphy of the Dovedale area, Derbyshire and Staffordshire. Quart. Journ. Geol. Soc., cv, 265.Google Scholar
Prentice, J. E., 1951. The Carboniferous Limestone of the Manifold valley region, North Staffordshire. Quart. Journ. Geol. Soc., cvi, 171.Google Scholar