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The Devonian–Carboniferous transition and its structural setting at Chillaton, West Devon, England

Published online by Cambridge University Press:  01 May 2009

E. B. Selwood ,
I. J. Stewart ,
P. J. Turner  and
M. J. Whiteley
E. B. Selwood
Affiliation:
Department of Geology, University of Exeter, North Park Road, Exeter EX4 4QE, England.
I. J. Stewart
Affiliation:
Department of Geology, University of Exeter, North Park Road, Exeter EX4 4QE, England.
P. J. Turner
Affiliation:
Department of Geology, University of Exeter, North Park Road, Exeter EX4 4QE, England.
M. J. Whiteley
Affiliation:
Department of Geology, University of Exeter, North Park Road, Exeter EX4 4QE, England.
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Summary

Boreholes penetrating the inverted limb of a major fold in an allochthonous thrust sheet at Chillaton, West Devon, revealed highly fossiliferous strata spanning the Devonian–Carboniferous boundary in continuous succession. Details of the fauna, which includes conodonts, trilobites and ostracods, are given. Abundant siphonodellid conodonts allow the boundary to be determined according to the recommendations of the working group on the Devonian–Carboniferous boundary of the IUGS Commission on Stratigraphy. The nature of the imbricate zone beneath the Main Thrust, in which the succession is situated, is described. In addition, the fabrics associated with thrusts which cut the olistostromic succession lower in the tectonic unit are discussed.

Type
Articles
Information
Geological Magazine , Volume 119 , Issue 4 , July 1982 , pp. 383 - 393
Copyright
Copyright © Cambridge University Press 1982

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