Search results for "Grafia"

showing 10 items of 4249 documents

Toward a Comprehensive Dam Monitoring: On-Site and Remote-Retrieved Forcing Factors and Resulting Displacements (GNSS and PS–InSAR)

2021

Many factors can influence the displacements of a dam, including water level variability and environmental temperatures, in addition to the dam composition. In this work, optical-based classification, thermal diachronic analysis, and a quasi-PS (Persistent Scatter) Interferometric SAR technique have been applied to determine both forcing factors and resulting displacements of the crest of the Castello dam (South Italy) over a one-year time period. The dataset includes Sentinel-1A images acquired in Interferometric Wide swath mode using the Terrain Observation with Progressive Scans SAR (TOPSAR); Landsat 8 Thermal Infrared Sensor (TIRS) thermal images, and Global Navigation Satellite System …

010504 meteorology & atmospheric sciencesLandsat TIRSScience0211 other engineering and technologiesTerrainSatellite system02 engineering and technologyForcing (mathematics)01 natural sciencesPS–InSARInterferometric synthetic aperture radarDam displacements Full graph GNSS Landsat TIRS PS–InSAR Sentinel-1A TOPSARSentinel-1A TOPSAR021101 geological & geomatics engineering0105 earth and related environmental sciencesRemote sensingdam displacementsGNSSQfull graphdam displacements; GNSS; Sentinel-1A TOPSAR; Landsat TIRS; PS–InSAR; full graphWater levelInterferometryGNSS applicationsGeneral Earth and Planetary SciencesSatelliteGeologySettore ICAR/06 - Topografia E CartografiaRemote Sensing
researchProduct

Secondary minerals from salt caves in the Atacama Desert (Chile): a hyperarid and hypersaline environment with potential analogies to the Martian sub…

2017

Over the past 15 years several expeditions by French, American and especially Italian cavers have unveiled over 50 caves in the Cordillera de la Sal (Atacama Desert, Northern Chile). Many of these caves contain a variety of speleothems and minerals, some of which have rarely been observed within karst systems. Most of the secondary deposits in these caves are composed of halite, but also other halide, carbonate, sulphate, nitrate, phosphate, and silicate minerals have been found. Among the sixteen cave mineral species recognized, atacamite, darapskite, blödite, leonite, anhydrite, and especially antarcticite are worth mentioning. In one of the samples an unknown Ca-Sr-bearing chloride miner…

010504 meteorology & atmospheric sciencesQH301-705.5Settore GEO/04 - Geografia Fisica E GeomorfologiaEarth scienceSalt (chemistry)martian010502 geochemistry & geophysics01 natural sciencesAstrobiologyatacamaCaveminerogenesisMinerogenesiBiology (General)Hyperaridity0105 earth and related environmental sciencesEarth-Surface Processescave mineralschemistry.chemical_classificationMartianQE1-996.5Settore GEO/06 - Mineralogiageographygeography.geographical_feature_categoryDesert (philosophy)Mars analoguesMars analogueCave mineralGeologysalt cavescave minerals atacama martianchemistrySalt cavecave minerals salt caves hyperaridity minerogenesis Mars analoguesGeologyInternational Journal of Speleology
researchProduct

How Offshore Groundwater Shapes the Seafloor

2018

The MARCAN project, launched last January, is working to fill a gap in our knowledge of how freshwater flowing underground shapes and alters the continental margins.

010504 meteorology & atmospheric sciencesSettore GEO/04 - Geografia Fisica E Geomorfologia010502 geochemistry & geophysics01 natural sciencesSeafloor spreadingOceanographyContinental margin13. Climate actioncontinental marginGeneral Earth and Planetary SciencesSubmarine pipelineGroundwaterGroundwaterGeology0105 earth and related environmental sciencesEos
researchProduct

Historical analysis of rainfall-triggered rockfalls: the case study of the disaster of the ancient hydrothermal Sclafani Spa (Madonie Mts, northern-c…

2017

Abstract. In 1851, the region of Sicily experienced many rainstorm-induced landslides. On 13 March 1851, a rainstorm brought about a severe rockfall disaster near the small town of Sclafani (Madonie Mountains, northern-central Sicily, Italy). Rocks detached from the carbonate crest of Mt Sclafani (813 m above sea level) and fell downslope, causing the collapse of the ancient hydrothermal spa (about 430 m above sea level) and burying it. Fortunately, there were no injuries or victims. Given its geological, geomorphological and tectonic features, the calcareous–dolomitic and carbonate–siliciclastic relief of Mt Sclafani is extremely prone to landsliding. This study combines the findings of de…

010504 meteorology & atmospheric sciencesSettore GEO/04 - Geografia Fisica E GeomorfologiaClimate change010502 geochemistry & geophysics01 natural scienceslcsh:TD1-1066Extreme weatherRockfalllcsh:Environmental technology. Sanitary engineeringNatural disasterlcsh:Environmental sciencesSea level0105 earth and related environmental scienceslcsh:GE1-350geographygeography.geographical_feature_categorylcsh:QE1-996.5Global warminglcsh:Geography. Anthropology. RecreationLandslideLandslide rainfall rockfall thermal spring Sicilylcsh:GeologyTectonicslcsh:GGeneral Earth and Planetary SciencesPhysical geographyGeologyNatural Hazards and Earth System Sciences
researchProduct

Disambiguating the soils of Mars

2020

Abstract Anticipated human missions to Mars require a methodical understanding of the unconsolidated bulk sediment that mantles its surface, given its role as an accessible resource for water and as a probable substrate for food production. However, classifying martian sediment as soil has been pursued in an ad hoc fashion, despite emerging evidence from in situ missions for current and paleo-pedological processes. Here we find that in situ sediment at Gusev, Meridiani and Gale are consistent with pedogenesis related to comminuted basalts mixing with older phyllosilicates – perhaps of pluvial origin – and sulfates. Furthermore, a notable presence of hydrated amorphous phases indicates signi…

010504 meteorology & atmospheric sciencesSettore GEO/04 - Geografia Fisica E GeomorfologiaEarth scienceWeatheringMartian soilRegolith01 natural sciences0103 physical sciencesWorld Reference Base for Soil ResourcesCryosol010303 astronomy & astrophysics0105 earth and related environmental sciencesUSDA soil taxonomyMartianSoil TaxonomyGelisolAstronomy and AstrophysicsSoil classificationMineral weatheringPedogenesisSettore AGR/14 - PedologiaSpace and Planetary ScienceSoil waterEnvironmental scienceWRBSettore M-GGR/01 - GeografiaPlanetary and Space Science
researchProduct

Geomorphological evolution of western Sicily, Italy

2017

Abstract This paper proposes a morphoevolutionary model for western Sicily. Sicily is a chain–foredeep–foreland system still being built, with tectonic activity involving uplift which tends to create new relief. To reconstruct the morphoevolutionary model, geological, and geomorphological studies were done on the basis of field survey and aerial photographic interpretation. The collected data show large areas characterized by specific geological, geomorphological, and topographical settings with rocks, landforms, and landscapes progressively older from south to north Sicily. The achieved results display: (1) gradual emersion of new areas due to uplift, its interaction with the Quaternary gl…

010504 meteorology & atmospheric sciencesSettore GEO/04 - Geografia Fisica E Geomorfologialcsh:QE1-996.5GeologySicily geomorphological evolution Quaternary uplift extensional tectonics down-cutting processes differential erosion.010502 geochemistry & geophysicsextensional tectonics01 natural sciencesdown-cutting processesQuaternarylcsh:GeologyPaleontologyupliftExtensional tectonicsdifferentialerosionQuaternarySicilyGeologygeomorphological evolution0105 earth and related environmental sciences
researchProduct

High-resolution 40Ar/39Ar chronostratigraphy of the post-caldera (<20 ka) volcanic activity at Pantelleria, Sicily Strait

2011

Abstract The island of Pantelleria (Sicily Strait), the type locality for pantellerite, has been the locus of major caldera-forming eruptions that culminated, ca. 50 ka ago, in the formation of the Cinque Denti caldera produced by the Green Tuff eruption. The post-caldera silicic activity since that time has been mostly confined inside the caldera and consists of smaller-energy eruptions represented by more than twenty coalescing pantelleritic centers structurally controlled by resurgence and trapdoor faulting of the caldera floor. A high-resolution 40Ar/39Ar study was conducted on key units spanning the recent (post-20 ka) intracaldera activity to better characterize the present-day status…

010504 meteorology & atmospheric sciencesSilicicForcing (mathematics)010502 geochemistry & geophysics01 natural sciencesPaleontologyGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)CalderaChronostratigraphy[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences40Ar/39Ar xenocrysts excess 40Ar anorthoclase[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereHorizon (geology)geographygeography.geographical_feature_categorySettore GEO/07 - Petrologia E PetrografiaSubsidencePaleosolSettore GEO/08 - Geochimica E VulcanologiaGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGeology
researchProduct

Phase equilibrium constraints on pre-eruptive conditions of recent felsic explosive volcanism at Pantelleria Island, Italy.

2010

International audience; We present experimental phase equilibria carried out on a pantelleritic bulk-rock composition with a peralkalinity index [PI = molar (Na2O + K2O)/Al2O3] = 1*4, which is representative of the most energetic pumice fall eruption of the resurgent post-caldera volcanism on Pantelleria island. For the explored conditions (P = 25-150 MPa; T = 680-800°C; H2Omelt up to 6 wt %; fO2 ≤ NNO, where NNO is nickel-nickel oxide buffer) clinopyroxene is the liquidus phase followed by alkali feldspar and then quartz. The crystallization of amphibole is limited to temperatures below 700°C. Aenigmatite crystallizes near the liquidus for P ≥ 100 MPa. When clinopyroxene is the sole liquid…

010504 meteorology & atmospheric sciencespantellerite[SDE.MCG]Environmental Sciences/Global Changeshydrous reduced magmaLiquidusengineering.material010502 geochemistry & geophysicsFeldspar01 natural sciencesPeralkaline rockAenigmatiteGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanologyphase equilibriaPetrologyGeomorphology0105 earth and related environmental sciencesMelt inclusionsFelsicSettore GEO/07 - Petrologia E PetrografiaGeophysics13. Climate actionvisual_artMagmaengineeringvisual_art.visual_art_mediumperalkaline magmatismAlkali feldsparGeologyPantelleria
researchProduct

Geology of Monte Gallo (Palermo Mts, NW Sicily)

2016

The promontory of Monte Gallo (Palermo, NW Sicily) is a spectacular site where Upper Triassic-Eocene carbonate platform rocks and Quaternary continental to marine deposits are well exposed. A Mesozoic-Paleogene rock succession allows the potential visitor to easily detect the features and the evolution of the Panormide carbonate platform, a shallow-water paleogeographic domain of the Southern Tethyan margin. Quaternary deposits, as well many landforms, enable the visitor to directly identify the interplay between climate changes, tectonics and fluctuations of marine level that occurred during the Quaternary Period. A detailed geological map (1:15,000 mapping scale) is presented, accompanied…

010506 paleontologyUpper Triassic-Eocene shallow-water carbonateSettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformSettore GEO/04 - Geografia Fisica E GeomorfologiaGeography Planning and Developmentquaternary continental and marine synthemClimate change010502 geochemistry & geophysics01 natural sciencesgeotourismPaleontologyEarth and Planetary Sciences (miscellaneous)GeotourismSicily0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryLandformGeological mapGeologic mapgeositeTectonicsQuaternaryScale (map)Geology
researchProduct

Multistratigraphic records of the Lower Cretaceous (Valanginian–Cenomanian) Puez key area in N. Italy

2016

Abstract We present a stratigraphic investigation of a Hauterivian to Cenomanian hemipelagic succession from Col Puez, in the Dolomites (Southern Alps, northern Italy). A composite section of seven segments was studied with bio-, magneto-, and chemostratigraphy, which enabled detailed and robust age calibration of the Puez succession. It also revealed the paleoceanographic history and helped identify the important global climatic events of that period. The age of the Lower Cretaceous Puez Formation in the Dolomites is refined as late Hauterivian to early Cenomanian. Ammonoids provide a detailed biostratigraphic subdivision that forms the basis for analyses of the faunal distribution and the…

010506 paleontologygeographyPlateaugeography.geographical_feature_categoryAptianPaleontology010502 geochemistry & geophysicsOceanography01 natural sciencesCretaceousPaleontologyChemostratigraphyFaciesPaleoclimatologyPeriod (geology)PALEOBIOGEOGRAFIACenomanianEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
researchProduct