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- W54512843 abstract "Publisher Summary The Alpine cycle consists of a succession of extensional phases that fragmented Pangea and were followed by a series of shortening phases due to the convergence of Africa with Europe that resulted in the formation of the Alpine fold belt. Each oceanic basin formation event was characterized by three phases: pre-rift, syn-rift, and post-rift. The duration of the Triassic transgressive half-cycle extended from the Early Triassic throughout half of the Middle Triassic. The short regressive interval that followed the peak of the Ladinian transgression was interrupted by a deformation event known as the “Carnian crisis.” In the entire Southern Alps, the latest Carnian and/or the earliest Norian were marked by renewed extensional tectonism that induced new subsidence and transgression. The Triassic long-term facies cycle can be subdivided into four second-order transgressive–regressive cycles. These four cycles are recorded in the Brianconnais and Piemont zones, but not in the external zones. The wide carbonate-dominated platform astride the future European and Apulia margins of the Ligurian Tethys was faulted everywhere by the end of the Norian. The chapter discusses the relationship of the Middle Triassic and Carnian extensional events to rifting of the Ligurian Tethys and Triassic paleogeography and the line of opening of the Ligurian Tethys in the Jurassic." @default.
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- W54512843 date "2011-01-01" @default.
- W54512843 modified "2023-09-23" @default.
- W54512843 title "The Age of the Onset of Tethyan Rifting in Western Europe" @default.
- W54512843 doi "https://doi.org/10.1016/s0928-2025(11)14005-5" @default.
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