Hostname: page-component-76fb5796d-5g6vh Total loading time: 0 Render date: 2024-04-27T00:35:11.877Z Has data issue: false hasContentIssue false
  • English
  • Français

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
Get access Rights & Permissions [Opens in a new window]

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

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

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