7 research outputs found
The tectonic puzzle of the Messina area (Southern Italy): Insights from new seismic reflection data
The Messina Strait, that separates peninsular Italy from Sicily, is one of the most seismically active areas of
the Mediterranean. The structure and seismotectonic setting of the region are poorly understood, although
the area is highly populated and important infrastructures are planned there. New seismic reflection data
have identified a number of faults, as well as a crustal scale NE-trending anticline few km north of the strait.
These features are interpreted as due to active right-lateral transpression along the north-eastern Sicilian
offshore, coexisting with extensional and right-lateral transtensional tectonics in the southern Messina
Strait. This complex tectonic network appears to be controlled by independent and overlapping tectonic
settings, due to the presence of a diffuse transfer zone between the SE-ward retreating Calabria subduction
zone relative to slab advance in the western Sicilian side
Coral Patch and Ormonde seamounts as a product of the Madeira hotspot, Eastern Atlantic Ocean
New detailed swath bathymetry and bottom samples from Coral Patch and Ormonde seamounts provide constraints on the emplacement of the Madeira hotspot in the Eastern Atlantic Ocean. Swath bathymetric data document that Coral Patch is a composite structure, made up of at least nine distinct volcanic centres. Lithified pelagic carbonates infilling fissures in lava blocks constrain a minimal age for the volcanism in the Early Miocene and represent the first documentation of Coral Patch acting as an offshore terrigenous-starved seamount. At Coral Patch, as already observed at the Ormonde seamount, volcanism was emplaced on top of a pre-existing relief resulting from the regional tectonic compressive regime
Post-breakup Compression in the Tyrrhenian Basin
AAPG European Regional Conference & Exhibition. Exploring The Mediterranean: New Concepts In An Ancient Seaway, 8-10 April 2013, Barcelona, SpainPeer reviewe
Styles and rates of deformation in the frontal accretionary wedge of the Calabrian Arc (Ionian Sea): controls exerted by the structure of the lower African plate
The Calabrian Arc is a narrow subduction-rollback system resulting from Africa/Eurasia plate
convergence. We analysed the structural style of the frontal accretionary wedge through a multiscale
geophysical approach. Pre-stack depth-migrated crustal-scale seismic profiles unravelled the
overall geometry of the subduction complex; high-resolution multi-channel seismic and sub-bottom
CHIRP profiles, together with morpho-structural maps, integrated deep data and constrained
the fine structure of the frontal accretionary wedge, as well as deformation processes along the
outer deformation front.
We identified four main morpho-structural domains in the western lobe of the frontal wedge:
the proto-deformation area at the transition with the abyssal plain; two regions of gentle and
tight folding; a hummocky morphology domain with deep depressions and intervening structural
highs; a highstanding plateau at the landward limit of the salt-bearing accretionary wedge,
where the detachment cuts through deeper levels down to the basement. Variation of
structural style and seafloor morphology in these domains are related to a progressively more
intense deformation towards the inner wedge, while abrupt changes are linked to inherited
structures in the lower African plate. Our data suggest focusing of intense shallow
deformation in correspondence of deeply rooted faults and basement highs of the incoming plate.
Back-arc extension in the Southern Tyrrhenian Sea has recently ceased, producing a
slowdown of slab rollback and plate-boundary re-organization along trans-tensional
lithospheric faults segmenting the continental margin. In this complex setting, it is not clear if the
accretionary wedge is still growing through frontal accretion. Our data suggest that shortening is
still active at the toe of the wedge, and uplift rates along single folds are in the range of
0.25-1.5 mm/yr. An unconformity within the Plio-Quaternary sediments suggests a discontinuity
in sedimentation and tectonic processes, i.e. a slowdown of shortening rate or an increase in
sedimentation rate, but not a real inactivation of frontal accretion, which still contribute