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The Lower Carboniferous Rocks of the Castle Hill Fault Block, Tenby, Pembrokeshire

Published online by Cambridge University Press:  01 May 2009

R. Sullivan
R. Sullivan
Affiliation:
Department of Geology, San Francisco State College, 1600 Holloway Avenue, San Francisco, California.
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Abstract

The rocks of Castle Hill previously considered to be of Tournaisian age are now shown to be referable to he Dibunophyllum Zone. The revised age greatly simplifies the structure of the fault block.

Type
Articles
Information
Geological Magazine , Volume 101 , Issue 2 , 17 April 1964 , pp. 113 - 115
Copyright
Copyright © Cambridge University Press 1964

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References

REFERENCES

Dixon, E. E. L., 1921. The country around Pembroke and Tenby. Mem. Geol. Surv., London.Google Scholar
Dixon, E. E. L., and Vaughan, A., 1912. The Carboniferous succession in Gower (Glamorganshire), with notes on its fauna and conditions of deposition. Quart. Jour. geol. Soc. London, 68, 477–571.Google Scholar