Search results for "EOF"

showing 10 items of 354 documents

Hydrogeological and geotechnical modeling of the foundation soils of Maredolce Lake in Palermo, aided by geophysical surveys

2019

The cultural heritage of Maredolce (Palermo) includes an Arab-Norman castle that originally stood on the shores of an artificial lake carved out of a basin dug out of the calcarenite and filled with water thanks to the channeling of the springs of San Ciro upstream. Subsequently, the lowering of the water table and the high hydraulic permeability of the outcropping rocks caused the lake to dry up. Recently, a project of enhancement of the cultural heritage required the restoration of the lake. The geophysical study presented here, including the integrated use of different techniques such as electrical and seismic tomography, Multichannel Analysis of the Surface Waves and ambient vibration r…

Seismic Refraction TomographyHVSRSettore GEO/11 - Geofisica ApplicataElectrical Resistivity TomographyMaredolce
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The integration of surface and subsurface stratigraphic data with HVSR measures for studies of seismic microzonation: the case of Oliveri (ME)

2013

Because of its high seismic hazard the urban area of Oliveri has been subject of a study on seismic microzonation at first level (OPCM 3907/2010). The urban area develops on a large coastal plain made of Late Pleistocene and Holocene mixed fluvial/marine sediments, that mainly consist of silty sands and gravels. The eastern part of this plain is dominated by the alluvial deposits of the Elicona torrent. The coastal and alluvial sediments overlap a complexly deformed substrate made of Hercynian metamorphites (Aspromonte unit), the Capo d’Orlando Flysch, the Antisicilide Argille Scagliose and Pleistocene clays and calcarenites. This area is affected by high uplift rates as recently estimated …

Seismic microzonation HVSR coastal plain sediments paleo-valleySettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/11 - Geofisica Applicata
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Seismic velocity structures of Southern Italy from tomographic imaging of the Ionian slab and petrological inferences.

2012

International audience; In this study we have determined detailed Vp and Vs seismic velocity models of the Ionian lithosphere subducting beneath the Tyrrhenian basin and of the surrounding mantle, by applying a post-processing technique to a large sample of local earthquake tomography studies. Our seismic velocity models permit us to infer the presence of low velocity anomalies within the slab, which we interpret as regions that are partially hydrated by fluids released during the subduction process. A petrological interpretation of the velocity anomalies gives new details on the magmatism of the volcanic Aeolian arc. Furthermore our velocity models provide a more detailed description of th…

Seismic tomography[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph][SDE.MCG]Environmental Sciences/Global ChangesSettore GEO/10 - Geofisica Della Terra SolidaSubduction zone processeSettore GEO/07 - Petrologia E Petrografia[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]crust and lithospherecrust and [Rheology]crust and lithosphere.crust and lithosphere. [Seismic tomography; Subduction zone processes; Rheology]Subduction zone processesRheology: crust and lithosphere.lithosphereRheology
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Integration of onshore and offshore seismic arrays to study the seismicity of the Calabrian Region: a two steps automatic procedure for the identific…

2014

Abstract. We plan to deploy in the Taranto Gulf some Ocean Bottom broadband Seismometer with Hydrophones. Our aim is to investigate the offshore seismicity of the Sibari Gulf. The seismographic network optimization consists in the identification of the optimal sites for the installation of the offshore stations, which is a crucial factor for the success of the monitoring campaign. In this paper, we propose a two steps automatic procedure for the identification of the best stations geometry. In the first step, based on the application of a set of a priori criteria, the suitable sites to host the ocean bottom seismic stations are identified. In the second step, the network improvement is eval…

SeismometerComputer simulationlcsh:Dynamic and structural geologySettore GEO/10 - Geofisica Della Terra Solidalcsh:QE1-996.5GeometryGeneral MedicineInduced seismicitylcsh:GeologyIdentification (information)lcsh:QE500-639.5Calabrian seismic network Netowork optimization Ocean Bottom Seismometer SeismicitySettore GEO/11 - Geofisica ApplicataBroadbandA priori and a posterioriSubmarine pipelinelcsh:Qlcsh:ScienceHost (network)GeologySeismologyAdvances in Geosciences
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Boschi di neoformazione in Italia: approfondimenti conoscitivi e orientamenti gestionali

2019

Nelle regioni meridionali, e in Sicilia in particolare, la fisionomia della vegetazione forestale post-abbandono è quella della macchia o arbusteto che difficilmente evolve verso un bosco propriamente detto. Il processo evolutivo della vegetazione spesso non raggiunge lo stadio di bosco non perché le condizioni ambientali non lo consentano ma per due ragioni fondamentali: i disturbi, in particolare gli incendi e il pascolo, e le limitazioni nell’arrivo di propaguli, causate dalla mancanza di piante madri, dei dispersori dei semi o entrambi. Infatti, in contesti favorevoli (assenza di disturbi e arrivo dei propaguli) la vegetazione evolve sino al bosco. Le formazioni preforestali frutto dei …

Settore BIO/07 - EcologiaMacchia mediterranea Boschi di neoformazione Successione secondaria Abbandono agricolturaSettore AGR/05 - Assestamento Forestale E Selvicoltura
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Geological modeling of Altavilla Milicia (Sicily) using HVSR data

2014

At today the use of inversion of HVSR curves is mainly limited to derive average parameters of the shear wave velocity, although recently they have been used also for a detailed reconstruction of the roof of the seismic bedrock (Di Stefano et al. 2014). Since ambient vibrations may contain waves travelling in all directions, as body waves and Rayleigh and Love waves, a limit of this method lies in the uncertain composition of seismic noise, in the lack of knowledge about the microseismic field and in the subjective choices regarding the data processing. This work aims to verify the potential and limits of the HVSR inversion for the purposes of geological reconstruction of the subsoil in hea…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaHVSR ellipticity shear wave velocity modelsSettore GEO/11 - Geofisica Applicata
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Evoluzione recente della linea di costa nel golfo di Palermo

2008

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaModificazioni recenti della linea di costa Golfo di Palermo spiagge di neoformazione
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A MESOZOIC PALEOMARGIN in WESTERN SICILY, its TERTIARY EVOLUTION and its PRESENT-DAY SEISMOGENETIC POTENTIAL

2013

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaPaleotectonic Sicily Seismic tomography Geotermal potential BeliceSettore GEO/03 - Geologia StrutturaleSettore GEO/11 - Geofisica Applicata
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Multivariate modelling of geophysical tomography data to identify a tectonized area

2018

An integrated analysis approach, based on geological investigations and 2D high-resolution shallow geophysical data, was proposed along a slope in the Bellolampo landfill area (Palermo, Italy) where the presence of a fault zone was hypothesized. Geophysical surveys included electrical resistivity tomography (ERT), induced polarization tomography (IPT) and seismic refraction tomography (SRT) techniques. The inversion of single geophysical parameter often does not allow to justify the complexity of the subsoil structures. The most appropriate solution should be to add additional physical or geological information so to get a constrained geological model. However, it is not at all easy to work…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/11 - Geofisica ApplicataElectrical resistivity tomography seismic refraction tomography còluster analysis tectonized area Bellolampo
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Studio per la definizione dei modelli concettuali dei corpi idrici sotterranei di Peloritani, Nebrodi e ragu-sano e indagini geofisiche correlate

2018

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/11 - Geofisica ApplicataPeloritani Nebrodi Ragusano idrogeologia geofisica geochimicaSettore GEO/08 - Geochimica E Vulcanologia
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