CINECA IRIS Institutional Research Information System
IRIS è la soluzione IT che facilita la raccolta e la gestione dei dati relativi alle attività e ai prodotti della ricerca. Fornisce a ricercatori, amministratori e valutatori gli strumenti per monitorare i risultati della ricerca, aumentarne la visibilità e allocare in modo efficace le risorse disponibili.
EnglishA detailed field survey, including structural and biostratigraphic analyses, has been integrated with sub-surface (seismic lines and well logs) data in order to reconstruct the stratigraphy, structure and tectonic evolution of the Colbordolo-Pesaro sector of the northern Apennines foothill zone (Marche region). The lithostratigraphic characters of the Miocene succession show a striking variability across three major (NW-SE elongated) structural ridges mapped within the study area. Major structures consist of faulted anticlines bounded by thrust ramps and backlimb backthrusts, separated by broader, open synclines, both involving a Mesozoic-Paleogene, mainly carbonate succession. The construction of a balanced and restored cross-section suggests that the complex shallow structures represent a geometrical requirement to the accommodation of the deep deformation.
| Titolo: | The Colbordolo-Pesaro area of the Romagna-Marche foothill zone (Northern Italian Apennines): stratigraphic and structural study | |
| Autori: | ||
| Data di pubblicazione: | 1995 | |
| Rivista: | ||
| Abstract: | A detailed field survey, including structural and biostratigraphic analyses, has been integrated with sub-surface (seismic lines and well logs) data in order to reconstruct the stratigraphy, structure and tectonic evolution of the Colbordolo-Pesaro sector of the northern Apennines foothill zone (Marche region). The lithostratigraphic characters of the Miocene succession show a striking variability across three major (NW-SE elongated) structural ridges mapped within the study area. Major structures consist of faulted anticlines bounded by thrust ramps and backlimb backthrusts, separated by broader, open synclines, both involving a Mesozoic-Paleogene, mainly carbonate succession. The construction of a balanced and restored cross-section suggests that the complex shallow structures represent a geometrical requirement to the accommodation of the deep deformation. | |
| Handle: | http://hdl.handle.net/11576/2301648 | |
| Appare nelle tipologie: | 1.1 Articolo su rivista |
File in questo prodotto:
Copyright © 2021