Rosenbaum, GideonLister, Gordon2015-12-080278-7407http://hdl.handle.net/1885/37185Reconstruction of the evolution of the Tyrrhenian Sea shows that the major stage of rifting associated with the opening of this basin began at ∼ 10 Ma. It involved two episodes of back arc extension, which were induced by the rollback of a west dippingKeywords: backarc basin; basin evolution; Cenozoic; slab; subduction; tectonic evolution; tectonics; Mediterranean Sea; Tyrrhenian Sea Apennines; Reconstruction; Sicilian Maghrebides; Subduction rollback; Tyrrhenian Sea200410.1029/2003TC0015182023-07-02