Search results for "geologia"

showing 10 items of 605 documents

Evidence of positive tectonic inversion in the north-central sector of the Sicily Channel (Central Mediterranean)

2016

In order to unravel the tectonic evolution of the north-central sector of the Sicily Channel (Central Mediterranean), a seismo-stratigraphic analysis of single- and multi-channel seismic reflection profiles has been carried out. This allowed to identify, between 20 and 50 km offshore the central-southern coast of Sicily, a ~80-km-long deformation belt, characterized by a set of WNW–ESE to NW–SE fault segments showing a poly-phasic activity. Within this belt, we observed: i) Miocene normal faults reactivated during Zanclean–Piacenzian time by dextral strike-slip motion, as a consequence of the Africa–Europe convergence; ii) releasing and restraining bend geometries forming well-developed pul…

Atmospheric SciencePiacenzian010504 meteorology & atmospheric sciencesSicily ChannelSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleInversion (geology)Structural basin010502 geochemistry & geophysics01 natural sciencesNappePush-up structureCompressive featuresEarth and Planetary Sciences (miscellaneous)Tectonic inversionForeland basinStrike-slip motion0105 earth and related environmental sciencesWater Science and TechnologyAnticlinePush-up structuresCompressive featureTectonicsSinistral and dextralCompressive features; Push-up structures; Seismic stratigraphy; Sicily Channel; Strike-slip motion; Tectonic inversion; Water Science and Technology; Atmospheric Science; Earth and Planetary Sciences (miscellaneous)SeismologyGeologySeismic stratigraphy
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Slope units-based flow susceptibility model: using validation tests to select controlling factors

2011

A susceptibility map for an area, which is representative in terms of both geologic setting and slope instability phenomena of large sectors of the Sicilian Apennines, was produced using slope units and a multiparametric univariate model. The study area, extending for approximately 90 km2, was partitioned into 774 slope units, whose expected landslide occurrence was estimated by averaging seven susceptibility values, determined for the selected controlling factors: lithology, mean slope gradient, stream power index at the foot, mean topographic wetness index and profile curvature, slope unit length, and altitude range. Each of the recognized 490 landslides was represented by its centroid po…

Atmospheric ScienceTopographic Wetness IndexSettore GEO/04 - Geografia Fisica E GeomorfologiaUnivariateSoil scienceLandslideLandslide susceptibility Univariate multiparametric model validation Mapping unitsCurvatureAltitudeSlope stability probability classificationStatisticsEarth and Planetary Sciences (miscellaneous)Range (statistics)Settore GEO/05 - Geologia ApplicataGeologyStream powerWater Science and Technology
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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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“Ragusa asphalt basin (Hyblean Plateau, Sicily): proposal of an ascent model from the deep oilfield”

2008

BACINO ASFALTIFERO TRASCORRENZA MODELLO ASCENSIONALESettore GEO/05 - Geologia Applicata
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“Proposta di recupero e fruizione delle miniere di roccia asfaltica di Ragusa (Sicilia sud-orientale)-

2008

BACINO MINERARIO ROCCIA ASFALTICA PROPOSTA DI RECUPEROSettore GEO/05 - Geologia Applicata
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Backthrusts and passive roof duplexes in fold-and-thrust belts. The case of Central-Western Sicily based on seismic reflection data

2012

Seismic reflection profiles crossing the area bounded by the M. Kumeta Ridge and the M. Maranfusa-M. Galiello-Rocca Busambra morphostructural feature (central-western Sicily) were used to constrain the deep structural setting of the Sicilian-Maghrebian fold-and-thrust belt (FTB). By integrating seismic, field and well data, we attempted to correlate outcropping and deep-seated contractional structures, shedding light on the internal geometries of the thrust system. Results of the new seismostratigraphic analysis presented in this paper reveal structural variations along the tectonic edifice. This suggests dividing the study area into two sectors: the western sector is characterized by forel…

BackthrustSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleDeep-seatedSeismostratigraphySicilian-Maghrebian fold-and-thrust beltDuplex
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Millstones as indicators of relative sea-level changes in northern Sicily and southern Calabria coastlines, Italy

2011

Abstract New data are presented for late Holocene relative sea-level changes in two coastal sites of Sicily and Calabria, southern Italy. Reconstructions are based on precise measurements of submerged archaeological remains that are valuable indicators of past sea-level position. The archaeological remains are millstone quarries carved on sandstone coastal rocks and nowadays partially submerged which, to the authors’ knowledge, are used for the first time as sea-level markers. Millstones of similar typology are located on the coast of Capo d’Orlando (northern Sicily) and Capo dell’Armi (southern Calabria). When the archeologically-based sea-level position is compared with the shoreline elev…

BeachrockShoregeographygeography.geographical_feature_categoryHolocenePleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaElevationtectonic movements; sea level changes; Holocene;tectonic movementArchaeologyMillstoneTectonicsgeoarcheologyPhysical geographysea level changeSicily and CalabriaSea levelHoloceneGeologyrelative sea-level changeEarth-Surface Processes
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Contribution of HVSR measures for seismic microzonation studies

2018

The HVSR method applied to seismic noise can be a very useful technique to map the site effects of the territory, to identify the thickness of the soft covering and so the depth of the seismic bedrock. The case of the urban area of Oliveri is presented. Because of its high seismic hazard this area has been subject of first level seismic microzonation. The town lies on a large coastal plain made of mixed fluvial/marine sediments, overlapping a deformed substrate. In order to identify points on the area probably suffering of relevant site effects and to define a preliminary Vs subsurface model, 23 HVSR measurements were performed. A clustering technique of continuous signals has been used to …

Bedrockgeographygeography.geographical_feature_categorySeismic microzonationHVSR010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaBedrockInversion (geology)FluvialClassification of discontinuitiesSeismic noise010502 geochemistry & geophysics01 natural sciencesGeophysicsSeismic hazardSettore GEO/11 - Geofisica ApplicataRange (statistics)Seismic microzonationCluster analysiSeismologyGeology0105 earth and related environmental sciences
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Théorie biblique de la cosmogonie et de la géologie : doctrine nouvelle fondéesur un principe unique et universel, puisé dans la Bible : ouvrage spéc…

1848

Bíblia i ciènciaBíblia i geologia
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Carbonate deposition and diagenesis in evaporitic environments: The evaporative and sulphur-bearing limestones during the settlement of the Messinian…

2015

The depositional and diagenetic processes involved in the formation of carbonates in the evaporitic environment of the Messinian Salinity Crisis are investigated in Southern Italy (Sicily and Calabria). Strong differences are observed between the studied sections that reflect specific depositional and diagenetic evolution in the interconnected sub-basins resulting from the syn-sedimentary tectonic fragmentation of the Central Sicilian and Calabrian domains. These carbonates formed diachronously in restricted perched sub-basins between the Tripoli Formation and the hypersaline settings of the MSC. The Calcare di Base (CdB) that can be interbedded with gypsum layers occurs rhythmically at the…

Calcare di BaseGypsumBacterial sulphate reductionSettore GEO/02 - Geologia Stratigrafica E Sedimentologica010504 meteorology & atmospheric sciencesEvaporiteGeochemistryDiagenetic carbonateSulphur LimestoneMineralogy[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]engineering.material010502 geochemistry & geophysicsOceanography01 natural scienceschemistry.chemical_compoundCelestineMessinian Salinity Crisis Carbonate SulphurEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesCalciteAnhydriteSettore GEO/07 - Petrologia E PetrografiaMessinian Salinity CrisiPaleontologySettore GEO/01 - Paleontologia E PaleoecologiaSettore GEO/08 - Geochimica E VulcanologiaDiagenesisEvaporitechemistryengineeringHaliteCarbonateGeology
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