| Přispěvatelé: |
S.G.I., Salvatore Critelli, Francesco Muto, Francesco Perri, Fabio Massimo Petti, Maurizio Sonnino, Alessandro Zuccari, Mastronuzzi, G., Artusa, C, Fontolan, Giorgio, Longo, D., Milella, M., Pignatelli, C., Piscitelli, A. |
| Popis: |
The integrated analysis of the geophysical, stratigraphic and geomorphological data collected in the Taranto seas, highlights the Holocene transgression that leads to the deposition of a considerable thickness of sandy-clay sediments, up to about 10 m thick, representing the body of marine terrace current in accumulation. They cover a sub-horizontal transgression surface shaped on the Plio- Pleistocene clays. The comparative analysis of sedimentary bodies and present depths confirm the current evolutionary model of the Tyrrhenian; in this time, between the sea surface and the bottom of that sea a depth equal to the difference between the shoreline and the recognized top of the sediment. |
