The Lower Carboniferous Rocks of the Castle Hill Fault Block, Tenby, Pembrokeshire
- 17 April 1964
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 101 (2) , 113-115
- https://doi.org/10.1017/s0016756800048548
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.Keywords
This publication has 2 references indexed in Scilit:
- Report On The Mosses From The Arctic BedQuarterly Journal of the Geological Society, 1912
- The Carboniferous Succession in Gower (Glamorganshire), with Notes on its Fauna & Conditions of DepositionQuarterly Journal of the Geological Society, 1911