Search results for "TECTONICS"

showing 10 items of 385 documents

Advanced radar-interpretation of InSAR time series for mapping and characterization of geological processes

2011

Abstract. We present a new post-processing methodology for the analysis of InSAR (Synthetic Aperture Radar Interferometry) multi-temporal measures, based on the temporal under-sampling of displacement time series, the identification of potential changes occurring during the monitoring period and, eventually, the classification of different deformation behaviours. The potentials of this approach for the analysis of geological processes were tested on the case study of Naro (Italy), specifically selected due to its geological setting and related ground instability of unknown causes that occurred in February 2005. The time series analysis of past (ERS1/2 descending data; 1992–2000) and current…

lcsh:GE1-350Series (stratigraphy)lcsh:QE1-996.5lcsh:Geography. Anthropology. RecreationInstabilityField (geography)Displacement (vector)InSAR; ground movements; multi-temporal measureslcsh:TD1-1066law.inventionlcsh:GeologyTectonicslcsh:GlawInterferometric synthetic aperture radarGeneral Earth and Planetary SciencesRadarTime serieslcsh:Environmental technology. Sanitary engineeringGeologySeismologylcsh:Environmental sciencesNatural Hazards and Earth System Sciences
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Tectonique salifère et déformation gravitaire de la marge passive sud-gabonaise de l'Albien au Turonien (secteur de Mayumba) Salt tectonic and thin-s…

2003

International audience; L'observation de données sismiques de bonne qualité relatives à la marge passive sud-gabonaise montre : 1) les structures extensives, compressives et inversives albo-turoniennes, associées à la tectonique gravitaire au-dessus du niveau salifère Ezanga (Aptien supérieur). D'est en ouest, ces structures synsédimentaires, d'échelle kilo-métrique, sont en blocs basculés, en anticlinaux, en roll over, en " carapace de tortue ", de nouveau en plis et failles inverses, et enfin en langues de sel déversées vers l'ouest. 2) l'influence du niveau salifère sur la structuration gravitaire ; 3) l'héritage passif syn-rift au niveau des zones hautes anté-salifères qui favorisent la…

marge passiveAlbian-Turonian.Albian-Turoniantectonique salifère[SDU.STU] Sciences of the Universe [physics]/Earth Sciences[ SDU.STU ] Sciences of the Universe [physics]/Earth Sciencessalt tectonicsdéformation gravitaireAlbo-turonien South Gabonthin skinned deformationpassive marginSud-Gabon
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First combined flux chamber survey of mercury and CO2 emissions from soil diffuse degassing at Solfatara of Pozzuoli crater, Campi Flegrei (Italy): M…

2014

Abstract There have been limited studies to date targeting gaseous elemental mercury (GEM) flux from soil emission in enriched volcanic substrates and its relation with CO 2 release and tectonic structures. In order to evaluate and understand the processes of soil–air exchanges involved at Solfatara of Pozzuoli volcano, the most active zone of Campi Flegrei caldera (Italy), an intensive field measurement survey has been achieved in September 2013 by using high-time resolution techniques. Soil–air exchange fluxes of GEM and CO 2 have been measured simultaneously at 116 points, widely distributed within the crater. Quantification of gas flux has been assessed by using field accumulation chamb…

mercury flux carbon dioxide soil degassinggeographygeography.geographical_feature_categorygenetic structuresMineralogychemistry.chemical_elementHydrothermal circulationMercury (element)Settore GEO/08 - Geochimica E VulcanologiaVolcanic mercurychemistry.chemical_compoundTectonicsGeophysicsFlux (metallurgy)chemistryImpact craterVolcanoCarbon dioxideGeochemistry and PetrologyCarbon dioxideCalderaSoil degassingMercury fluxSolfataraGeology
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Orthogonal switching of AMS axes during type-2 fold interference : Insights from integrated X-ray computed tomography, AMS and 3D petrography

2017

We applied X-ray computed microtomography (μ-CT) in combination with anisotropy of magnetic susceptibility (AMS) analysis to study metamorphic rock fabrics in an oriented drill core sample of pyrite-pyrrhotite-quartz-mica schist. The sample is extracted from the Paleoproterozoic Martimo metasedimentary belt of northern Finland. The μ-CT resolves the spatial distribution, shape and orientation of 25,920 pyrrhotite and 153 pyrite grains localized in mm-thick metapelitic laminae. Together with microstructural analysis, the μ-CT allows us to interpret the prolate symmetry of the AMS ellipsoid and its relationship to the deformation history. AMS of the sample is controlled by pyrrhotite porphyro…

microtomography010504 meteorology & atmospheric sciencesMetamorphic rockMineralogyCore sampleengineering.material010502 geochemistry & geophysics01 natural sciencesstrainAMSAnisotropyPyrrhotite0105 earth and related environmental sciencesrasitusta114SchistGeologyFold (geology)Ellipsoidmagnetic fabricpyrrhotiteengineeringmicrotectonicsGeologyPrincipal axis theorem
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Dynamics of hydrofracturing and permeability evolution in layered reservoirs

2015

International audience; A coupled hydro-mechanical model is presented to model fluid driven fracturing in layered porous rocks. In the model the solid elastic continuum is described by a discrete element approach coupled with a fluid continuum grid that is used to solve Darcy based pressure diffusion. The model assumes poro-elasto-plastic effects and yields real time dynamic aspects of the fracturing and effective stress evolution under the influence of excess fluid pressure gradients. We show that the formation and propagation of hydrofractures are sensitive to mechanical and tectonic conditions of the system. In cases where elevated fluid pressure is the sole driving agent in a stable tec…

reservoir[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Materials Science (miscellaneous)Effective stressfluid pressureBiophysicsGeneral Physics and AstronomyPattern formation[SDU.STU]Sciences of the Universe [physics]/Earth Sciencesreservoirsstresshydrofracturesfluid pressure4Ultimate tensile strength[PHYS.MECA.SOLID]Physics [physics]/Mechanics [physics]/Solid mechanics [physics.class-ph][PHYS.MECA.MEFL]Physics [physics]/Mechanics [physics]/Fluid mechanics [physics.class-ph]Physical and Theoretical ChemistryPorosityMathematical PhysicsCauchy stress tensorPhysicsMechanicssimulationreservoirs2lcsh:QC1-999TectonicsPermeability (earth sciences)Keywords: hydrofractures1simulation3Relative permeabilityhydrofractureGeologystress5lcsh:Physics
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Integrated analyses of syn-tectonic basin fill to costrain the deformation evolution in a fold thrust belt: field examples from the sicilian chain

2011

sedimentary basins synsedimentary tectonics Sicily late Miocene early Pliocene
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Seismotectonics in the North-Western Sicily Continental Margin: implications for Geohazard assessment

2017

Active processes in the Northern Sicily Continental Margin (NSCM) have been analysed to produce a seismotectonic map, in order to obtain a useful tool for the assessment of the seismic hazard of the sea-land region. The seismotectonic map is composed of overlapping layers that represent the distribution of different features, such as lithostratigraphy, tectonic elements, seismicity, heat flow, gravimetry, magnetometry, Moho depth, horizontal and vertical movements, submarine landslides, fluid emissions, outlining the mutual relationship and the active structures. The NSCM is suitable to test this approach because it’s located in a transitional area between the Sicilian-Maghrebian chain to t…

seismotectonics seismicity active tectonics Geohazard
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SEISMOTECTONIC MAP OF THE NORTHERN SICILY CONTINENTAL MARGIN (NSCM) AND IMPLICATIONS FOR GEOHAZARD ASSESSMENT

2018

The Sicily dominates the central Mediterranean Sea. The Northern Sicily Continental Margin (NSCM) is a segment of the Appeninic-Tyrrhenian System whose upbuilding refers to both the postcollisional convergence between Africa and a very complex “European” crust (Bonardi et al., 2001) or AlKaPeKa (sensu Boullin, 1986) and the opening of the Tyrrhenian back-arc basin. Seismostratigraphic and structural analysis of a large number of available (from ViDePi project) and unpublished (from Department of Earth and Marine Science of the University of Palermo) multichannel seismic reflection profiles acquired across the NSCM, allow us to produce an accurate seismotectonic map, in order to obtain a use…

seismotectonics seismicity active tectonics Geohazard
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Stress sensitivity of stylolite morphology

2009

International audience; Stylolites are rough surfaces that form by localized stress-induced dissolution. Using a set of limestone rock samples collected at different depths from a vertical section in Cirque de Navacelles (France), we study the influence of the lithostatic stress on the stylolites morphology on the basis of a recent morphogenesis model. We measured the roughness of a series of bedding-parallel stylolites and show that their morphology exhibits a scaling invariance with two self-affine scaling regimes separated by a crossover-length (L) at the millimeter scale consistent with previous studies. The importance of the present contribution is to estimate the stylolite formation s…

self-affine scalingMorphology (linguistics)010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]MineralogyMagnitude (mathematics)morphogenesisSurface finish010502 geochemistry & geophysics01 natural sciencesStress (mechanics)Geochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryEarth and Planetary Sciences (miscellaneous)Geotechnical engineeringpaleo-stressScaling0105 earth and related environmental sciencesroughness[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsDeformation (mechanics)stylolitesStress fieldGeophysicsSpace and Planetary ScienceStyloliteGeology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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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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