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• W68753011 abstract "The Iberian Peninsula is a good example of late Hercynian structures that influenced Mesozoic sedimentation. Complex graben systems, evolving along the fracture systems during late Hercynian movements were filled by hundreds of meters of red beds during the Permian and Triassic, the final stages of Hercynian movements were accompanied by several magmatic events. This paper deals with some well studied areas of the Iberian Peninsula (Cantabrian Mountains, Pyrenees, Catalo-nian ranges, Central System margins, Iberian ranges and southern margin of the Iberian massif) where basin evolution and tectonic activity are clearly related. A model for the evolution of the Iberian ranges is proposed based in Alvaro et al. (1979) with three distinct periods: (1) a compressive regime related to late Hercynian movements and the formation of Pangea, which occurred from the Late Carboniferous to Early Permian (Autunian); (2) a less-well-defined period when Saxonian facies were deposited; and (3) a distensive regime resulting in rift-basin development and Buntsandstein sedimentation, followed by marine sediments as the Tethys Sea encroached on the margins of the Iberian massif. This third period lasted from the Late Permian (Thuringian) to, at least, the Early Jurassic." @default.
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• W68753011 date "1988-01-01" @default.
• W68753011 modified "2023-10-09" @default.
• W68753011 title "Permian and Triassic rift basins of the Iberian Peninsula" @default.
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• W68753011 doi "https://doi.org/10.1016/b978-0-444-42903-2.50036-1" @default.
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