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- Received 19 September 2018
- Revision received 18 January 2019
- Accepted 24 January 2019
- Published 12 March 2019.
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© 2019 The Author(s). Published by The Geological Society of London. All rights reserved
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Regione Toscana (Italy)
Enzo Mantovani
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How and why the present tectonic setting in the Apennine belt has developed
- Article
- Abstract
- Late Miocene: first least-action tectonic reorganization in the central Mediterranean area (decoupling of the Adria plate from Africa)
- Early Pleistocene: second tectonic reorganization (internal deformation, with uparching and dextral torsion, of the Adria plate)
- Middle Pleistocene: third tectonic reorganization (the Adria plate accelerates, reactivating tectonic activity in the surrounding belts)
- Discussion
- Conclusions
- Acknowledgements
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