Search results for "southern tyrrhenian"

showing 7 items of 27 documents

Plio-Quaternary tectonic evolution offshore the Capo Vaticano Promontory

2014

We reconstruct the Plio-Quaternary tectono-stratigraphic evolution in the offshore Capo Vaticano (W Calabria, Italy) by integrating data obtained from single- and multi-channel reflection seismic profiles and a reprocessed version of the CROP M2A/III line. NW-trending, high-angle normal faults, dipping ~70° to the south-west formed along the continental slope connecting the south-west continental shelf of the Capo Vaticano Promontory to the Gioia Tauro Basin (Pepe et al., 2014). Faults generally have small displacements up to 40 m and are sealed by Pleistocene deposits. West of the Capo Vaticano promontory and in the Gioia Basin, a SE-dipping, normal fault system, more than 32 km long, is r…

Southern Tyrrhenian Sea Capo Vaticano Plio-QuaternarySettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia Strutturale
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Rifted margin formation in the South Tyrrhenian Sea: A high resolution profile across the North Sicily passive continental margin.

2000

A new, 150 km long seismic line across the continental margin of north Sicily has been acquired and interpreted. The overall structure of the margin is controlled by extension, which caused crustal thinning and widespread normal faulting. Two main thinned zones are observed in the south in correspondence with the Cafalù basin and farther to the north at the continent-ocean transition. Zones of thinned crust coincide with zones of intense normal faulting. Extension began in late Tortonian times and caused the opening of the Cefalù basin controlled by a northward dipping listric fault. Messinian stretching affected most of the future margin and provoked a widening of the Cefalù basin and norm…

geographygeography.geographical_feature_categoryRiftPleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaCrustFault (geology)Structural basinSouthern Tyrrhenian North Sicily continental margin Rifted Continental Margin Cefalù basin./dk/atira/pure/sustainabledevelopmentgoals/life_below_waterPaleontologyGeophysicsContinental marginGeochemistry and PetrologyLithospherePassive marginSDG 14 - Life Below WaterGeologySeismology
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First assessment of the epifauna associated with macroalgae of the vermetid reef along the coasts of Favignana Island (South Tyrrhenian Sea)

2017

With this study we provide a first baseline assessment of the epifauna associated with the macroalgae of the vermetid reefs present along the coasts of the Island of Favignana (Egadi Islands Marine Protected Area, Italy). A total of 14 taxa were identified. Epifaunal assemblages differed according to structure and composition of algal communities. The amphipod group presented the highest number of individuals. The tubicolous species Ampithoe ramondi Audouin, 1826 (Ampithoidae) was the most abundant species.

macroalgaesouthern Tyrrhenian SeaSettore BIO/02 - Botanica Sistematicavermetid reef.Fauna biodiversitySettore BIO/05 - ZoologiaFavignana Island
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New seismological and geological-structural contributions to the support of a seismotectonic model of the hinge area between northern Sicily and sout…

2012

seismotectonicSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleSettore GEO/11 - Geofisica Applicatasouthern tyrrhenianNorthern sicily continental marginneotectonic
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Submarine Slope Failures Along the Northern Sicilian Continental Margin (Southern Tyrrhenian Sea) and Possible Implications for Geo-Hazard

2013

Mass wasting and downslope movements are common processes that have contributed to shape the northern Sicilian continental margin (southern Tyrrhenian Sea) since the Late Quaternary. Nevertheless, processes controlling their evolution are still partially unknown and a variety of geologic factors can be responsible for their formation. In this work we present an overview of the main mass wasting features (submarine canyons, landslides, debris flows) observed and mapped in different sectors of the northern Sicilian margin. The margin is characterized by a narrow, steep continental shelf (1-2°) and a very irregular and steep (6-8°) upper slope. The main aims of this work are: (1) to outline th…

southern Tyrrhenian Seageographygeography.geographical_feature_categorySettore GEO/02 - Geologia Stratigrafica E SedimentologicaLandslideSubmarine canyonMass wastingsubmarine slope failurelanguage.human_languagePaleontologyTectonicsContinental marginlanguageSubmarine pipelineQuaternaryslope failure swath bathymetry geohazard southern Tyrrheniangeo-hazardSicilianGeomorphologyGeology
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Submarine canyon of the north-western Sicilian offshore (Southern Tyrrhenian Sea): variability in morphologies, sedimentary processes and tectonic se…

2013

southern Tyrrhenian Seasubmarine canyonSettore GEO/02 - Geologia Stratigrafica E Sedimentologicamarine geomorphology
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Morphological and structural analysis of the Ustica Island offshore (southern Tyrrhenian Sea) for the definition of the marine geological hazard

2008

ustica island multibeam echosounder volcanism southern tyrrhenian sea submarine geomorphology
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