| Přispěvatelé: |
Yamada Y., Kawamura K., Ikehara K., Ogawa Y., Urgeles R., Mosher D., Chaytor J., Strasser M., Ogata, K., Tinterri, R., Pini, GIAN ANDREA, Mutti, E., Ogata K., Tinterri R., Pini G.A., Mutti E. |
| Popis: |
Within the Eocene-Oligocene syn-orogenic deposits of the Epiligurian succession (Northern Apennines of Italy), a field-based study of the Specchio Unit (lower Rupelian) reveals that this complex is made up by the amalgamation of 3 distinct mass-transport deposits (MTDs), the largest of which reaches a maximum volume of ca. 75 km3. These bodies deposited inside a complex, intraslope basin system, developed atop the submerged Ligurian accretionary prism at the collision with the Adria continental plate. The MTDs originated from catastrophic retrogressive collapses starting from the upper slope and involving progressively shallow-water environments, from distal shelfal pro-delta and delta-front sediments up to proxi-mal coastal fan-delta deposits. These recurrent and close in time, catastrophic slope failures were probably caused by tectonic and climatic triggers, such as the enhanced tectonic activity due to incipient Apenninic continental collision and the onset of harsh climatic conditions, as suggest by oxygen isotopic maxima (e.g. Oi-1a event). Although the wedge toe/foredeep system are considered the principal loci of mass transport development, usually located in deep-water settings, here we stress the importance of catastrophic mass transport events also atop the wedge, in shallow-water depositional domains. Mass transport processes also have a fundamental role in reshaping the upper physiographic profile of an evolving ac-cretionary wedge. The correct interpretation of such mass transport processes has also important implications for geohazard forecasting in modern active continental margins, for example in terms of tsunamigenic potential. |
