Search results for "grafica"
showing 10 items of 553 documents
An active oblique-contractional belt at the transition between the Southern Apennines and Calabrian Arc: The Amendolara Ridge, Ionian Sea, Italy
2014
High-resolution, single-channel seismic and multibeam bathymetry data collected at the Amendolara Ridge, a key submarine area marking the junction between the Apennine collision belt and the Calabrian subduction forearc, reveal active deformation in a supposedly stable crustal sector. New data, integrated with existing multichannel seismic profiles calibrated with oil-exploratory wells, show that middle to late Pleistocene sediments are deformed in growth folds above blind oblique-reverse faults that bound a regional pop-up. Data analysis indicates that similar to 10 to 20km long banks that top the similar to 80km long, NW-SE trending ridge are structural culminations above en echelon fault…
Sequence stratigraphy of the Late Neogene – Quaternary deposits in the Egadi Islands offshore (NW Sicily)
2008
Carbonate Platform/Basin system during the Mesozoic: stratigraphic evolution, erosional surfaces and sequence stratigraphy framework
2011
Preliminary results of a crustal seismic profile across Sicily (Italy)
2008
Some considerations on the results of the crustal SIRIPRO profile in central Sicily
2013
Geological results of the crustal SIRIPRO transect in central Sicily
2013
Slope failures along the northern Sicilian continental margin (southern Tyrrhenian sea)
2009
Seismically-induced soft-sediment deformation structures in Upper Triassic deepwater carbonates (Central Sicily)
2016
We describe soft-sediment deformation structures into the Upper Triassic cherty limestone outcropping in the Pizzo Lupo section (Central Sicily, Italy), pertaining to the deep-water palaeodomain of the Southern Tethyan margin. In the study section, mainly consisting of thin-bedded mudstone/marl alternations with bedded chert intercalations, some lithofacies have been separated on the basis of the abundance of the calcium carbonate/clay content and the overall textural features. The deformational structures, displaying different deformational styles as folded and faulted beds, disturbed layers, clastic dikes, and slumps occur mainly in the deformed horizons that involve marl-dominated lithof…