Hostname: page-component-7bb8b95d7b-5mhkq Total loading time: 0 Render date: 2024-09-13T14:55:32.675Z Has data issue: false hasContentIssue false
  • English
  • Français

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
Get access Rights & Permissions [Opens in a new window]

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

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Bond, G., 1950. The Lower Carboniferous reef limestones of Cracoe, Yorkshire. Quart. Journ. Geol. Soc., cv, 157.Google Scholar
Kendall, P. F., and Wroot, H. E., 1924. The Geology of Yorkshire.Google Scholar
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