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The Age and Relationships of the Cornbrook Sandstone

Published online by Cambridge University Press:  01 May 2009

D. G. Jones  and
T. R. Owen
D. G. Jones
Affiliation:
Department of Geology, King's College, London, W.C. 2.
T. R. Owen
Affiliation:
Department of Geology, University College, Swansea, Glam.
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Abstract

The Cornbrook Sandstone of Titterstone Clee Hill has plants of Westphalian (Middle Coal Measures) age. It is thus probably a correlative of the lower Kinlet Group of the Forest of Wyre. The base is unconformable to the Old Red Sandstone and Carboniferous Limestone while the top is apparently conformable with Productive Coal Measures of the Sweet Coal Group, also of Middle Coal Measures age.

Type
Articles
Information
Geological Magazine , Volume 98 , Issue 4 , August 1961 , pp. 285 - 294
Copyright
Copyright © Cambridge University Press 1961

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References

REFERENCES

Crookall, R., 1939. The Plant Break in the Carboniferous Rocks of Britain. Bull. Geol. Surv., No. 1, 13–26.Google Scholar
Dineley, D. L. and Gossage, D. W., 1959. The Old Red Sandstone of the Cleobury Mortimer Area, Shropshire. Proc. Geol. Assoc., lxx, 221–239.CrossRefGoogle Scholar
Dixon, E. E. L., 1910. The Geology of the Titterstone Clee Hills. Geol. Mag., xlvii, 458–460.CrossRefGoogle Scholar
Dixon, E. E. L., 1917. The Geology of the Titterstone Clee Hill Coal Field. Trans. Roy. Soc. Edinb., li, 1064–1071.Google Scholar
George, T. N., 1956. The Namurian Usk Anticline. Proc. Geol. Assoc., lxvi, 297–316.CrossRefGoogle Scholar
Jones, D., 1871. On the Co-relation of the Carboniferous Deposits of Cornbrook, Brown Clee, Harcott and Coalbrook-dale. Geol. Mag. viii, 363.CrossRefGoogle Scholar
Kidston, R., 1917. The Fossil Plants of Titterstone Clee Hill Coal Field. Trans. Roy. Soc. Edinb., li, 1071–1084.Google Scholar
Newell Arber, E. A., 1913. On the Fossil Floras of the Wyre Forest with Special Reference to the Neighbouring Coal Measure Areas. Phil. Trans. Roy. Soc. London B, cciv.Google Scholar
Prestwich, J., 1840. On the Geology of Coalbrook-dale. Trans. Geol. Soc., Ser 2, v., 413–CrossRefGoogle Scholar
Trueman, A. E. in Marshall, C. E., 1942. Field Relations of certain of the Basic Igneous Rocks associated with the Carboniferous strata of the Midland Counties. Quart. Journ. Geol. Soc., xcviii, 1–20.Google Scholar
Vaughan, A., 1905. The Palaeontological Sequence in the Carboniferous Limestone of the Bristol Area. Quart. Journ. Geol. Soc., lxi, 181–307.CrossRefGoogle Scholar
Whitehead, T. H. and Pocock, R. W., 1947. Dudley and Bridgnorth. Mem. Geol. Surv.Google Scholar