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The Caledonides of the Anglo-Brabant Massif reviewed

Published online by Cambridge University Press:  01 May 2009

T. C. Pharaoh ,
S. G. Molyneux ,
R. J. Merriman ,
M. K. Lee  and
J. Verniers
T. C. Pharaoh
Affiliation:
British Geological Survey, Keyworth, Nottingham NG12 5GG, U.K.
S. G. Molyneux
Affiliation:
British Geological Survey, Keyworth, Nottingham NG12 5GG, U.K.
R. J. Merriman
Affiliation:
British Geological Survey, Keyworth, Nottingham NG12 5GG, U.K.
M. K. Lee
Affiliation:
British Geological Survey, Keyworth, Nottingham NG12 5GG, U.K.
J. Verniers
Affiliation:
Geologisch Instituut, Universiteit Gent, B–9000, Belgium
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Extract

The Anglo–Brabant Massif has formed a positive structural element since the Acadian orogenic phase in mid–Devonian times. As a consequence, the Caledonian basement lies at relatively shallow depth across the massif, encompassing a large area of southern Britain, the southern North Sea, southern Netherlands, Belgium and northern France (Fig.1).

Type
Articles
Information
Geological Magazine , Volume 130 , Issue 5 , September 1993 , pp. 561 - 562
Copyright
Copyright © Cambridge University Press 1993

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References

Andre, L., Herbosch, A., Vanguestaine, M. & Verniers, J. 1991. Proceedings of the International Meeting on the Caledonides of the Midlands and the Brabant Massif. Annales de la Société Géologique de Belgique 114, 1–282.Google Scholar