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- W2061567249 abstract "The recent fault system of eastern Sicily can be identified in the Peloritan Mountains, in particular where it cross-cuts carbonate ranges in areas preserved from strong torrential erosion. The scarp of the Mount Kalfa fault results from normal sinistral slip at a mean rate of 0.9 mm·yr−1 during the Würm to Present east-west extension. This normal fault belongs to the Apenninico-Calabro-Sicilian rift zone that cross-cuts the Tyrrhenian arc. Its Sicilian and Apenninic segments enable characterization of a Middle-Late Pleistocene change of the stress regime that could have occurred during a steepening without subduction of the Ionian slab (along Calabria) and its lateral detachment. Le système de failles récentes Est-Sicilien peut être reconnu dans les massifs carbonatés des monts Péloritains. La morphologie du relief de faille du mont Kalfa, avec son escarpement holocène, est liée à son mouvement normal sénestre de 0,9 mm·an−1 durant une extension est-ouest, du Würm à l'Actuel. Cette faille normale appartient à la ceinture extensive apennino-calabro-sicilienne, qui découpe l'arc Tyrrhénien. Dans les segments siciliens et apenniniques de cette dernière, nous pouvons mettre en évidence un changement au Pléistocène moyen-supérieur du régime de contraintes, qui pourrait accompagner l'arrêt de la subduction avec verticalisation du slab ionien et sa rupture latérale." @default.
- W2061567249 created "2016-06-24" @default.
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- W2061567249 date "1999-11-01" @default.
- W2061567249 modified "2023-10-04" @default.
- W2061567249 title "Morphologie et cinématique d'une faille holocène dans les monts Péloritains (Sicile) ; implications géodynamiques" @default.
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- W2061567249 doi "https://doi.org/10.1016/s1251-8050(00)88494-3" @default.
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