Sedimentation in the Northern Apennines–Corsica tectonic knot (Northern Tyrrhenian Sea, Central Mediterranean): offshore drilling data from the Elba–Pianosa Ridge
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- 作者：Gianluca Cornamusini (1) (2)
Vincenzo Pascucci (3) - 关键词：Stratigraphy ; Petrography ; Turbidite system ; Geodynamic setting ; Northern Tyrrhenian Sea
- 刊名：International Journal of Earth Sciences
- 出版年：2014
- 出版时间：April 2014
- 年：2014
- 卷：103
- 期：3
- 页码：821-842
- 全文大小：4,793 KB
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Vincenzo Pascucci (3)
1. Dipartimento di Scienze Fisiche, della Terra e dell’Ambiente, Università di Siena, Siena, Italy
2. Centro di Geotecnologie, Università di Siena, S. Giovanni V.no, Italy
3. Dipartimento di Scienze della Natura e del Territorio, Università di Sassari, Sassari, Italy - ISSN：1437-3262
文摘
The Northern Tyrrhenian Sea is located on the collisional zone between the Alpine Corsica and the Northern Apennines and is a key area for gaining a better understanding of the complex relationships between these two systems. The knowledge of the wide offshore part of this zone, located between Corsica (France) and mainland Italy, is based primarily on the analysis of several seismic profiles tied to the outcropping geology and unpublished preliminary reports of few offshore wells. The here presented study of two offshore wells provides a revision of the sedimentology, biostratigraphy and petrography of the thick, mainly siliciclastic, Tertiary successions (about 3,600?m) composing the Elba–Pianosa Ridge (EPR), a structural/morphological high separating the Tuscan Shelf to the east from the Corsica Basin to the west. A comparison with similar deposits cropping out in the surrounding onshore areas (Northern Apennines, Corsica, Tuscan Archipelago, Piedmont Tertiary Basin) provides additional constraints for refinement of the complex geodynamic and regional setting in which the EPR evolved.