Large deep-seated gravitational slide off Ischia volcanic island, EasternTyrrhenian sea (Italy)

Research output: Contribution to conferenceOther

Abstract

Ischia island develops at the edge of the shelf area and represents the sub-aerial section of a larger, E-W trendingvolcanic ridge including others submerged or buried volcanic edifices. In the past decade the island’s offshorehas been the object of extensive hydrographic and marine geophysical surveys that have shown the structuralcomplexity of the undersea sections and have overall shown the importance of gravity failures in island’s evolution.In this paper we report a previously unreported deep-seated slump structure and associated surficial mass wastingphenomena which occur off Ischia south-western flank. Recently acquired hydrological and geophysical data leadto identify the morphological features and the internal organization of the failed sediments which spread alongthe continental slope. The extent of this deep-seated deformations and the deep structural levels involved lead toinvestigate on the influence played by volcanic processes and regional tectonics on slope failure.The Ischia southern slope was explored through a multibeam survey and a single-channel seismic survey.Acquisition was carried out from aboard the R/V Urania at depths between 400 and 1200 m. The bathymetric datawere collected using a hull mounted Reson 8160 multibeam sonar. Resolution resulted in a 20x20 m implementedwith 50x50 gridded size provided by a previously collected data. Seismic survey consisted of 6 seismic lines runalong the slope spaced 1 km between them and 5 cross lines. The acoustic source used was a 1Kjoule high-energypower supply system with a multi-tips (400) sparker array, fired at 2s time interval.The collected data show that a wide submerged area of 350 km2, between 400 to 1200 m depths is undergoingslow-moving deformation and associated secondary mass wasting phenomena. Morphological features includetrenches, counterscarps, bulging and both extensional and contractional features while internal deformations showtypical landward dipping reflectors with strong evidence of synsedimentary faulting and asymmetric anticlines.Deformation processes operate at various scales generating folds with wavelength ranging from hundreds meters to kilometers. Extensional and rotational rupture surfaces sole out at various low-angle detachment planes locatedat depths from few hundreds meters to 1 kilometer in subsurface.
Original languageEnglish
Number of pages0
Publication statusPublished - 2014

    Fingerprint

Cite this