Abstract
The major subdivisions in the Variscan of the Armorican Massif are based either upon the Paleozoic faunas and sedimentary successions or upon the tectonometamorphic and geodynamic evolution of the different zones or terranes.
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Reference
Cogné J (1986) La chaîne hercynienne ouest-européenne correspond-elle à un orogène par collision? Propositions pour une interprétation géodynamique globale. Colloq Int CNRS 268: 111–129
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© 1994 Springer-Verlag Berlin Heidelberg
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Paris, F., Robardet, M. (1994). The Variscan. In: Chantraine, J., Rolet, J., Santallier, D.S., Piqué, A., Keppie, J.D. (eds) Pre-Mesozoic Geology in France and Related Areas. IGCP-Project 233. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-84915-2_8
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DOI: https://doi.org/10.1007/978-3-642-84915-2_8
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-84917-6
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