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Three Palaeozoic sequences belonging to three different basins crop out in the Calabrian–Peloritan Arc. Their age covers the time span from middle (?) Cambrian to early Carboniferous. The sequences comprise terrigenous, volcanic and carbonate rocks, and show low‐grade metamorphism. The basement is of pre‐middle Cambrian age, crops out in the Calabrian–Peloritan Arc, and was metamorphosed prior to the opening to the Palaeozoic basins. The Palaeozoic basins existed no later than the middle Carboniferous, with inferred maximum crustal extension in the Cambro‐Ordovician. By Devonian time, the tectonic regime was compressional overall with middle Devonian island‐arc type volcanic activity that continued until the closure of the basins. Approximately 330 Myr, the Palaeozoic sequences experienced low‐pressure greenschist facies metamorphism and continuing subduction controlled the Variscan tectonogenesis with 280 Myr island‐arc type intrusive magmas. Subduction ceased and late‐stage 280–270 Myr granitic magmas were emplaced during continental collision. The crustal sector carrying the Palaeozoic basins is interpreted as comprising fragments of an active continental margin, one of the several microplates, located at the southern margin of the Euro‐Asia continent which faced a large (at least 1500 km in width) ocean basin.

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