New data for the kinematic interpretation of the Alps-Apennines junction (Northwestern Italy). (Articolo in rivista)

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  • 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
  • Mosca P.; Polino R.; Rogledi S.; Rossi M. (2010)
    New data for the kinematic interpretation of the Alps-Apennines junction (Northwestern Italy).
    in International journal of earth sciences (1999, Print)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Mosca P.; Polino R.; Rogledi S.; Rossi M. (literal)
Pagina inizio
  • 833 (literal)
Pagina fine
  • 849 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 99 (literal)
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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