The Origin of the Supposed Tufa Bands in Carboniferous Reef Limestones-Reference-Cited by-同舟云学术

The Origin of the Supposed Tufa Bands in Carboniferous Reef Limestones

Published:1952-06 Issue:3 Volume:89 Page:195-200
ISSN:0016-7568
Container-title:Geological Magazine
language:en
Short-container-title:Geol. Mag.

Author:

Black W. W.

Abstract

ABSTRACTThin 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.

Publisher

Cambridge University Press (CUP)

Subject

Geology

Reference4 articles.

1. The Lower Carboniferous reef limestones of Cracoe, Yorkshire;Bond;Quart. Journ. Geol. Soc.,1950

2. The stratigraphy of the Dovedale area, Derbyshire and Staffordshire;Parkinson;Quart. Journ. Geol. Soc.,1950

3. Kendall P. F. , and Wroot H. E. , 1924. The Geology of Yorkshire.

4. The Carboniferous Limestone of the Manifold valley region, North Staffordshire;Prentice;Quart. Journ. Geol. Soc.,1951

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