Scheda di dettaglio – i prodotti della ricerca
| Dato | Valore |
|---|---|
| Title | The interplay between mantle convective motions and the structural evolution of the Central-Northern Apennines |
| Abstract | The Central Apennines consist of a fold and thrust belt developed during Neogene, involving sedimentary successions of different paleogeographic domains. The geodynamic evolution of this sector was controlled by several important tectonic events, highlighted by numerous depositional sequences recognized in the Neogene marine successions. The time scanning of the stratigraphic events allowed to be reconstruct: the different stages of the eastward shifting of the chain-foredeep-foreland system; the deformation chronology; the more recent effects of the interactions between the regional uplift and extensional tectonics in the chain and the progressive eastward tilting of the Periadriatic sector. The Neogene foredeep and thrust top basins of the Central Apennines are filled by siliciclastic deposits from a Tyrrhenian crystalline area. The most important tectono- stratigraphy events developed during Messinian-Early Pliocene. |
| Source | Rendiconti online Società Geologica Italiana 3, pp. 208–209 |
| Keywords | mantle interactioncentral appenninetectonic evolutioncentral italy |
| Journal | Rendiconti online Società Geologica Italiana |
| Editor | Società Geologica Italiana, Roma, Italia |
| Year | 2008 |
| Type | Articolo in rivista |
| Authors | Centamore E.; Rossi D. |
| Text | 424565 2008 Scopus 2 s2.0 75349091434 mantle interaction central appennine tectonic evolution central italy The interplay between mantle convective motions and the structural evolution of the Central Northern Apennines Centamore E.; Rossi D. Dipartimento Scienze della Terra, Universita di Roma la Sapienza, P.le A. Moro 5, 00185 Roma, , Italy The Central Apennines consist of a fold and thrust belt developed during Neogene, involving sedimentary successions of different paleogeographic domains. The geodynamic evolution of this sector was controlled by several important tectonic events, highlighted by numerous depositional sequences recognized in the Neogene marine successions. The time scanning of the stratigraphic events allowed to be reconstruct the different stages of the eastward shifting of the chain foredeep foreland system; the deformation chronology; the more recent effects of the interactions between the regional uplift and extensional tectonics in the chain and the progressive eastward tilting of the Periadriatic sector. The Neogene foredeep and thrust top basins of the Central Apennines are filled by siliciclastic deposits from a Tyrrhenian crystalline area. The most important tectono stratigraphy events developed during Messinian Early Pliocene. 3 Published version http //www.scopus.com/record/display.url eid=2 s2.0 75349091434 origin=inward Articolo in rivista Societa Geologica Italiana 2035 8008 Rendiconti online Societa Geologica Italiana Rendiconti online Societa Geologica Italiana Rendiconti online Soc. Geol. Ital. Rendiconti online Societa Geologica Italiana. Rendiconti online SGI Rendiconti online SGI, note brevi Rendiconti online della Societa Geologica Italiana david rossi ROSSI DAVID |