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The rifting of the Tyrrhenian Basin
Authors:F Trincardi  N Zitellini
Institution:(1) Istituto per la Geologia Marina, Consiglio Nazionale delle Ricerche, 40127 Bologna, Italy
Abstract:An evolved system of North-South trending rotational normal faults records the direction of a stretching event on the Tyrrhenian Sea continental margins.Evolutionary stages of a typical rifted basin are recognized in the Tyrrhenian Sea through the interpretative analysis of seismic data, A major unconformity marks the end of a quite short (Tortonian to middle-Pliocene) rifting phase. However, no well-developed drift-related structures are seen to be active during the deposition of the post-rift sequence.
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