Chaîne varisque
Open Access

Fig. 1


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Tectonic map of the Variscan belt in Western Europe. Continental terranes, Avalonia, Saxo-Thuringia, Armorica-Barandia, Brunia, are separated by ophiolitic sutures, namely the Rheic suture and the Medio-European suture, to the north and south of Armorica respectively. The internal zone of the Variscan belt comprises high-grade nappes overlying a parautochtonous unit belonging to the northern margin of Gondwana.

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