Middle Oligocene Extension in the Mediterranean Calabro-Peloritan Belt (Southern Italy)
Middle Oligocene extension in the Mediterranean Calabro-Peloritan belt (Southern Italy). Insights from the Aspromonte nappes-pile. Thomas Heymes, Jean-Pierre Bouillin, Arnaud Pecher, Patrick Monié, R. Compagnoni To cite this version: Thomas Heymes, Jean-Pierre Bouillin, Arnaud Pecher, Patrick Monié, R. Compagnoni. Middle Oligocene extension in the Mediterranean Calabro-Peloritan belt (Southern Italy). Insights from the Aspromonte nappes-pile.. Tectonics, American Geophysical Union (AGU), 2008, 27, pp.TC2006. 10.1029/2007TC002157. hal-00283182 HAL Id: hal-00283182 https://hal.archives-ouvertes.fr/hal-00283182 Submitted on 29 May 2008 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Middle Oligocene extension in the Mediterranean Calabro-Peloritan belt (Southern 2 Italy). Insights from the Aspromonte nappes-pile. 3 4 Heymes, T., Bouillin, J.-P., Pêcher, A., Monié, P. & Compagnoni, R. 5 6 Abstract 7 The Calabro-Peloritan belt constitutes the eastward termination of the southern segment 8 of the Alpine Mediterranean belt. This orogenic system was built up during the convergence 9 between the Eurasian and the African plates, roughly directed North-South since the Upper 10 Cretaceous. It was subsequently fragmented during the opening of the Western Mediterranean 11 basins since Oligocene times.
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