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The Western Tuscany, in the inner sector of the Northern Apennines, is characterized by a thinned continental crust (∼20–25km), high heat flow (>100mWm−2), and the presence of magmatism. The latter produces the current geothermal activity, which is mostly localized at the large Larderello–Travale field settled above the granites with the same name. These features and the several Late Miocene sedimentary...
We examine the tectonic evolution and structural characteristics of the Quaternary intermontane Mugello, Casentino, and Sansepolcro basins, in the Northern Apennines fold-and-thrust belt. These basins have been classically interpreted to have developed under an extensional regime, and to mark the extension-compression transition. The results of our study have instead allowed framing the formation...
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