http://www.cnr.it/ontology/cnr/individuo/prodotto/ID6621
Four-dimensional tectono-stratigraphic evolution of the Southeasternperi-Tyrrhenian Basins (Margin of Calabria, Italy) (Articolo in rivista)
- Type
- Label
- Four-dimensional tectono-stratigraphic evolution of the Southeasternperi-Tyrrhenian Basins (Margin of Calabria, Italy) (Articolo in rivista) (literal)
- Anno
- 2009-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1016/j.tecto.2009.02.030 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- A. Milia; E. Turco; P.P. Pierantoni; A. Schettino (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#altreInformazioni
- Ten years after the Umbria-Marche earthquake, Central Italy (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
- http://www.sciencedirect.com/science/article/pii/S0040195109001206 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
- Note
- ISI Web of Science (WOS) (literal)
- Scopus (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Istituto per l'Ambiente Marino Costiero, CNR, Calata Porta di Massa, Porto di Napoli, 83, 80133, Naples, Italy
Dipartimento di Scienze della Terra, Università di Camerino, Via Gentile III da Varano, 62032, Camerino, Italy (literal)
- Titolo
- Four-dimensional tectono-stratigraphic evolution of the Southeasternperi-Tyrrhenian Basins (Margin of Calabria, Italy) (literal)
- Abstract
- We use seismic reflection profiles of diverse resolutions integrated with high resolution bathymetry and
calibrated by deep wells, piston cores and field data to derive a structural and stratigraphic interpretation of
the Southeastern peri-Tyrrhenian Basins. The study area is located in the Southeastern Tyrrhenian Sea
offshore Calabria. We document a tectono-stratigraphic evolution of the sedimentary basins from the
Serravallian to the Present. The basins formation started during the Serravallian and the area was
successively affected by EW normal faulting and approximately NS transfer faults in the Messinian
Lower Pleistocene time range. During the Lower Pleistocene the tectonic depressions, completely filled
with sediments, were affected by folding associated with transcurrent tectonics along a NW-trending left
lateral fault. Finally, during the Middle Pleistocene, a change in the slip direction produced minor pull-apart
basins that overprinted the folds. The basin analysis revealed the stratigraphic signature of the tectonic
events and, the uplifting and subsiding areas and the direction from which sediments arrive into the
tectonic depression. The four-dimensional geologic reconstruction of the Margin of Calabria furnished new
constrains for the kinematic evolution of the Southeastern peri-Tyrrhenian Basins. We suggest that the
superposition of different structural styles reflects a variation of the relative velocity between the Southern
Apennine Arc and the Calabria Arc during the formation of the Apennine Thrust Belt. (literal)
- Prodotto di
- Autore CNR
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