In the Armorican Massif, at the end of the Devonian, all the oceanic spaces are closed and the collision process has already started.
CITATION STYLE
Rolet, J., Gresselin, F., Jegouzo, P., Ledru, P., & Wyns, R. (1994). Intracontinental Hercynian Events in the Armorican Massif. In Pre-Mesozoic Geology in France and Related Areas (pp. 195–219). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-642-84915-2_20
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