http://www.cnr.it/ontology/cnr/individuo/prodotto/ID29796
New data for the kinematic interpretation of the Alps-Apennines junction (Northwestern Italy). (Articolo in rivista)
- Type
- Label
- New data for the kinematic interpretation of the Alps-Apennines junction (Northwestern Italy). (Articolo in rivista) (literal)
- Anno
- 2010-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s00531-009-0428-2 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Mosca P.; Polino R.; Rogledi S.; Rossi M. (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#note
- In: International Journal of Earth Sciences, vol. 99 (4) pp. 833 - 849. Springer, 2010. (literal)
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Pietro Mosca (corresponding author)
CNR - Institute of Geosciences and Earth Resources, Via Valperga Caluso 35, 10125 Torino, Italy
Riccardo Polino
CNR - Institute of Geosciences and Earth Resources, Via Valperga Caluso 35, 10125 Torino, Italy
Sergio Rogledi
ENI-E&P Division, Southern Europe Exploration, Via Emilia 1, 20097 San Donato Milanese (MI), Italy
Massimo Rossi
ENI-E&P Division, Geoscience Technical Services, Via Emilia 1, 20097 San Donato Milanese (MI), Italy (literal)
- Titolo
- New data for the kinematic interpretation of the Alps-Apennines junction (Northwestern Italy). (literal)
- Abstract
- Alps and Apennines are juxtaposed within an approximately 100 km-wide area covered by the Upper Eocene to Miocene successions of the Tertiary Piedmont Basin. The Upper Eocene-Oligocene evolution of this area was characterized to the north and west by the propagation of the SE-verging Southalpine thrust-fold belt that can be traced from the Po Plain subsurface until the Torino Hill-Saluzzese area, and to the south by a high-angle, broadly E-W oriented megashear zone that led to the juxtaposition of different crustal levels and controlled the development of a mosaic of partly independent sub-basins. Since the latest Oligocene the N-verging Apenninic tectonics prevailed in the collisional system and the Tertiary Piedmont Basin evolved as a wide thrust-top basin, bounded to the north by the N-verging Monferrato arc and characterized by a tectono-sedimentary evolution recording changes of subsidence and shift of depocentres in relation to crustal structures. (literal)
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