Caledonian and late Caledonian Europe: a working hypothesis involving two contrasted compressional/extensional scenarios
DOI:
https://doi.org/10.3989/egeol.90463-4453Keywords:
Caledonian, late Caledonian, extensional province, inversion tectonicsAbstract
The tectonomagmatic and metamorphic structuration of the European Caledonian realm suggests that two mutually perpendicular compressional/extensional scenarios developed during the Ordovician-Devonian time-span. As a result of the mid Ordovician Grampian compressional scheme (Caledonian s.s.), a major extensional province developed further east from the Caledonian foldbelt in continental Europe. This scenario ended by early/mid Devonian, with the complete locking of North America, Baltica and Gondwana into a Pangaea supercontinent, thus triggering a contrasted tectonic environment which might be termed
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