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- W2023326037 abstract "Abstract The Tyrrhenian Basin has developed as a marginal basin through drifting of the Calabrian-Sicilian arc system towards the east-southeast. The main structural features of the basin result from this movement. The tensional structures (normal faults) of the margins are mainly aligned N10° to N30°E; the transform faults are oriented N110°–N120°E. Except for a previous structuralization linked to the Western Mediterranean rifting and drifting, the first extensional movements affected the Tyrrhenian area as early as Lower Miocene time, during the post-Burdigalian. Nevertheless, the main rifting phase which led to oceanic accretion was initiated during the Late Tortonian. The narrow central oceanic area, generated mainly around the Early Pliocene, is restricted to the rift's axis. The marginal basin type of evolution of the Tyrrhenian Sea is most probably directly linked to subduction of the Ionian lithosphere. Nevertheless, interferences between collision in the surrounding Apennines, Calabria or Sicilides and subduction processes have dominated this special back-arc basin evolution. Since Late Tortonian time, the Tyrrhenian arc shows a regional N120°E-oriented tensional pattern. Short compressional events occur briefly in Middle Pliocene and Middle Pleistocene times, correlated with brief paroxysmal phases of extension and subsidence. The deformation depends on the presence of a subduction zone parallel to the Calabrian arc swell which allows the migration of the unblocked segments of the arc in a N120°E direction." @default.
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- W2023326037 date "1987-01-01" @default.
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- W2023326037 title "Structural evolution of the Tyrrhenian back-arc basin" @default.
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- W2023326037 doi "https://doi.org/10.1016/0025-3227(87)90010-7" @default.
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