Search results for "Ionian"

showing 10 items of 25 documents

Active tectonics along the south east offshore margin of Mt. Etna: New insights from high-resolution seismic profiles

2018

The offshore margin of Mt. Etna has been shaped by Middle Pleistocene to Holocene shortening and extension and, more recently, by gravity-related sliding of the volcanic edifice. These processes have acted contemporaneously although the gravitational component largely prevails over the tectonic one. In order to investigate this issue, we focused on the main role of active tectonics along the south-eastern offshore of Mt. Etna by means of marine high-resolution seismic data. Seismic profiles revealed post-220 ka sedimentary deposits unconformably overlaying the Lower-Middle Pleistocene Etnean clayey substratum and volcanics of the Basal Tholeiitic phase and the Timpe phase. Offshore Aci Trez…

010504 meteorology & atmospheric sciencesPleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia Strutturaleactive tectonics010502 geochemistry & geophysics01 natural sciencesSicilian thrust-beltPaleontologyActive tectonicActive tectonics; Ionian Sea; Mt. Etna; Seismic investigation; Sicilian thrust-belt; Earth and Planetary Sciences (all)Seismic investigationHolocene0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryContinental shelfMt. Etnalcsh:QE1-996.5Fold (geology)Ionian SeaMt. Etna; seismic investigation; active tectonics; Sicilian thrust-belt; Ionian SeaSeafloor spreadingVolcanic rocklcsh:GeologyTectonicsGeneral Earth and Planetary SciencesSedimentary rockEarth and Planetary Sciences (all)Geology
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Distribution of REEs in box-core sediments offshore an industrial area in SE Sicily, Ionian Sea: Evidence of anomalous sedimentary inputs

2009

The distribution of rare earth elements and yttrium (REEs+Y) has been investigated in box-core sediments recovered from four stations in the Sicilian coastal zone seawards of Augusta, one of the most industrialized and contaminated areas in the Mediterranean region. Shale-like REE patterns and low Y/Ho ratios (close to the chondritic ratio) suggest a dominant terrigenous (geogenic) source for REE. Slight enrichment of LREE over the HREE is interpreted as due to preferential adsorptive transfer of LREE from seawater to sediment particles. Samples from offshore cores exhibit slightly positive Gd and negative Ce anomalies. It is here hypothesized that main drivers of anthropogenic Gd flux towa…

Geologic SedimentsEnvironmental EngineeringHealth Toxicology and MutagenesisOceans and SeasGeochemistryFluxMineralogyIndustrial WasteGadoliniumGeologic SedimentsMediterranean seaEnvironmental ChemistrySicilyRare earth elements Ce anomaly Gd anomaly Box-core sediment Offshore Ionian SeaTerrigenous sedimentPublic Health Environmental and Occupational HealthSedimentGeneral MedicineGeneral ChemistryCeriumPollutionSettore GEO/08 - Geochimica E VulcanologiaSeawaterSedimentary rockMetals Rare EarthBayGeologyWater Pollutants ChemicalEnvironmental Monitoring
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Preliminary data concerning the morphology of a Calabrian Ionian margin area: Caulonia and Marina di Gioiosa canyons

2008

In the framework of the Vector National Italian Project (VulCost line), aimed to study the role of the morphology and the geology of the Ionian Calabrian margin in the coastline evolution, an oceanographic cruise was planned to collect geophysical data along two canyon systems: Caulonia and Marina di Gioiosa. The survey explored the continental shelf and slope from a depth of 15 m to more than 1150 m, using Multibeam Echosounder to investigate the seafloor topography. This work provides an outline of the erosive feature of the slope, shaped mostly by seasonal river input and by the connection to the structural and geological characteristics of the margin, made interesting by a narrow shelf …

CanyonShoregeographygeography.geographical_feature_categoryEcologyContinental shelfIonian Calabrian MarginGEO/04 - GEOGRAFIA FISICA E GEOMORFOLOGIASubmarine canyonseafloor topographySeafloor spreadingPaleontologyTectonicsOceanographyContinental marginmorphologyGeneral Earth and Planetary SciencesQuaternaryIonian Calabrian Margin seafloor topography morphologyEcology Evolution Behavior and SystematicsGeologyGeneral Environmental ScienceChemistry and Ecology
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A Mediterranean Monk Seal Pup on the Apulia coast (Southern Italy): sign of an ongoing recolonisation?

2020

The Mediterranean monk seal (Monachus monachus) is one of the most endangered marine mammals in the world. This species has been threatened since ancient times by human activities and currently amounts to approximately 700 individuals distributed in the Eastern Mediterranean Sea (Aegean and Ionian Sea) and Eastern Atlantic Ocean (Cabo Blanco and Madeira). In other areas, where the species is considered “probably extinct”, an increase in sporadic sightings has been recorded during recent years. Sightings and accidental catches of Mediterranean monk seals have become more frequent in the Adriatic Sea, mainly in Croatia but also along the coasts of Montenegro, Albania and Southern Italy. A Med…

0106 biological sciencesSeal (emblem)Mediterranean climateAdriatic SeaEndangered speciesSettore BIO/05 - ZoologiaMonachus monachusmitochondrial DNA010603 evolutionary biology01 natural sciencesMediterranean monk sealMonachus monachuGreek islandMontenegrolcsh:QH301-705.5Nature and Landscape Conservation<i>Monachus monachus</i>Ecologybiology010604 marine biology & hydrobiologyEcological Modelingendangered speciesbiology.organism_classificationAgricultural and Biological Sciences (miscellaneous)FisheryGeographylcsh:Biology (General)Threatened speciesIonian island
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Active tectonics in the Calabrian Arc: Insights from the Late Miocene to Recent structural evolution of the Squillace Basin (offshore eastern Calabri…

2023

The Calabrian Arc represents one of the most active sectors of the upper plate of the Tyrrhenian-Ionian subduction system. This research aims to reconstruct the evolution of the Squillace Basin (Ionian offshore of the Calabrian Arc) from the Late Miocene to Recent times and recognise active shallow and deep structures using a multiscale approach. The latter is based on interpreting high-penetration and high-resolution seismic reflection profiles, calibrated with well-log data coupled with bathymetric data and the distribution of instrumental earthquakes. Data highlight three steps in the evolution of the Squillace Basin. A Late Miocene extensional event led to the formation of WNW-ESE orien…

GeophysicsSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleActive tectonics Strike-slip tectonics Calabrian Arc (Italy) Ionian Sea Tyrrhenian SeaEarth-Surface Processes
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Neogene to Quaternary evolution of the Calabrian Subduction System, (Central Mediterranean)

2009

We construct an ESE striking to WNW geological cross-section across the Calabrian Subduction System (Central Mediterranean) using seismic near vertical profiles and field data. The interpreted profiles were time-to-depth converted, merged and translated in a geological section stretching from the Marsili Oceanic Basin (Southern Tyrrhenian Sea) to the Ionian accretionary complex . Moving toward the east, the resulting section through the Paola, Amantea, and Crati basins, the Coastal Chain and Sila Massif and Crotone basin. The maximum elongation of these basins change progressively moving toward the east: from NNW in the Paola to NS in the Crati to the NNE in the Crotone basins. Data we pres…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleIonian subduction zone Central Mediterranean
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An anomalous case in the evolution of the Mesozoic sedimentary basins between Alpine and Ionian Tethys: the Panormide Carbonate Platform (Sicily).

2007

Mesozoic sedimentary basins Alpine and Ionian Tethys Panormide Carbonate Platform Sicily
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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…

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicaseismic reflection profilessouthern Italyblind fault segment modelingSettore GEO/03 - Geologia StrutturaleAmendolara Ridge Ionian SeaActive fault-related folds; Blind fault segment modeling; Ionian basin; Seismic reflection profiles; Southern italyactive fault-related foldsIonian Basin
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Spazio e lingua nella 'costruzione' greca dell'identità etnica. Alcune osservazioni a partire da Erodoto

2018

The paper aims to offer an account of some representative opinions of ancient Greeks about the role of the space, conceived in its geographical/environmental value, in which a certain population lives, as well as of the language spoken by a population, in order to build historically the concept of Greek nation (to Hellenikón). The different positions expressed on these matters by Herodotus, Thucydides, Strabon and Pausanias are discussed, and the examination mostly concernes the ethnic and historical-linguistic aspects of the representation of the Dorians and Ionians.

space/environmentEthnic identityhistory of Greek languageDorians Ionians PelasgiansSettore L-FIL-LET/02 - Lingua E Letteratura Greca
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Seismic stratigraphy of upper Quaternary shallow-water contourite drifts in the Gulf of Taranto (Ionian Sea, southern Italy)

2018

Abstract The occurrence of articulated seafloor morphology over continental shelf-upper slope environments, may result in a significant change in the patterns and intensity of basin-scale thermohaline circulation during eustatic sea-level fluctuations. These changes may cause, in turn, erosion, deposition and/or transport of sediments at the seafloor, to form shallow-water contourite drifts. Here we investigate this process in the NW sector of the Gulf of Taranto (Ionian Sea) during and following the Last Glacial Maximum (LGM), by integrating multibeam bathymetric data, ultra-high resolution seismic-reflection data and gravity core data. Sea level fall caused subaerial exposure of the summi…

Axial and lateral channel-patch drifts; Channel-related drifts; Gulf of Taranto; Ionian Sea; Last Glacial Maximum; Shallow-water contourites; Younger DryasYounger Dryas010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleGulf of TarantoAxial and lateral channel-patch driftsYounger Drya010502 geochemistry & geophysicsOceanography01 natural sciencesChannel-related driftsPaleontologyGeochemistry and PetrologyShallow-water contouriteShallow-water contouritesYounger DryasSea level0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryLast Glacial MaximumContinental shelfAxial and lateral channel-patch driftGeologyContouriteLast Glacial MaximumIonian SeaSeafloor spreadingThermohaline circulationChannel-related driftQuaternaryGeology
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