Search results for "flu"

showing 10 items of 16583 documents

A dust-enshrouded tidal disruption event with a resolved radio jet in a galaxy merger

2018

Tidal disruption events (TDEs) are transient flares produced when a star is ripped apart by the gravitational field of a supermassive black hole (SMBH). We have observed a transient source in the western nucleus of the merging galaxy pair Arp 299 that radiated >1.5 × 10 erg at infrared and radio wavelengths but was not luminous at optical or x-ray wavelengths. We interpret this as a TDE with much of its emission reradiated at infrared wavelengths by dust. Efficient reprocessing by dense gas and dust may explain the difference between theoretical predictions and observed luminosities of TDEs. The radio observations resolve an expanding and decelerating jet, probing the jet formation and evol…

010504 meteorology & atmospheric sciencesGeneral Science & TechnologyInfraredAstronomyAstrophysics::High Energy Astrophysical PhenomenaFOS: Physical sciencesAstrophysics::Cosmology and Extragalactic AstrophysicsAstrophysicsGalaxy merger01 natural sciencesTidal disruption eventGravitational fieldMD Multidisciplinary0103 physical sciencesAstrophysics::Solar and Stellar AstrophysicsCOREBLACK-HOLES010303 astronomy & astrophysicsAstrophysics::Galaxy Astrophysics0105 earth and related environmental sciencesHigh Energy Astrophysical Phenomena (astro-ph.HE)PhysicsJet (fluid)Supermassive black holeta115Science & TechnologyMultidisciplinaryAstrophysics - Astrophysics of GalaxiesGalaxyMultidisciplinary SciencesWavelengthAstrophysics of Galaxies (astro-ph.GA)Science & Technology - Other TopicsAstrophysics::Earth and Planetary AstrophysicsAstrophysics - High Energy Astrophysical PhenomenaEMISSIONSTARS
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The river harbour of Ostia Antica - stratigraphy, extent and harbour infrastructure from combined geophysical measurements and drillings

2018

Abstract We performed a combined geophysical and geoarchaeological survey of the harbour of ancient Ostia, Italy, to investigate the extent of the former harbour basin, the sedimentary infill and possible building remains around the harbour. Besides geoarchaeological results the paper highlights the advantage of combining vibracore drilling with different geophysical prospection methods, which are sensitive to different physical soil parameters. Geophysical methods applied were electrical resistivity tomography (ERT), ground penetrating radar (GPR) and seismics with shear and compressional waves. The extent and shape of the harbour basin were determined by ERT profiling. The ERT profiles we…

010504 meteorology & atmospheric sciencesGeoarchaeologyFluvialGeophysicsStructural basin010502 geochemistry & geophysics01 natural sciencesCoringHarbourGround-penetrating radarSedimentary rockElectrical resistivity tomographycomputerGeomorphologyGeology0105 earth and related environmental sciencesEarth-Surface Processescomputer.programming_languageQuaternary International
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Noble gas magmatic signature of the Andean Northern Volcanic Zone from fluid inclusions in minerals

2021

Trace volatile elements like He are key for understanding the mantle source signature of magmas and to better constrain the relative roles of subduction and crustal processes to the variability of along-arc chemical and isotopic signatures of magmatic fluids. Here we report on noble gas abundances and isotopic data of Fluid Inclusions (FIs) in eruptive products and/or fumarolic gases from the Colombia-Ecuador segment of Andean Northern Volcanic Zone (NVZ). FIs in olivine phenocrysts from Ecuador (El Reventador, Cotopaxi and Tungurahua) yield air-normalized corrected He-3/He-4 ratios of 7.0-7.4 R-A, within the MORB range (8 +/- 1 R-A). With exception of the Cotopaxi lavas (opx = 50 km at the…

010504 meteorology & atmospheric sciencesGeochemistryAndean Volcanic Belt Helium voclanic gases Crustal thickness Fluid inclusions Helium Noble gases Northern Volcanic Zoneengineering.material010502 geochemistry & geophysics01 natural sciencesHeliumMantle (geology)Noble gaseGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyCrustal thickneFluid inclusions[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentVolatilesFluid inclusions0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryOlivineSubductionGeologyNorthern Volcanic ZoneFluid inclusionNoble gasesCrustal thicknessVolcanoAndean Volcanic BeltengineeringPhenocrystGeology
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Quantitative models of hydrothermal fluid–mineral reaction: The Ischia case

2013

Abstract The intricate pathways of fluid–mineral reactions occurring underneath active hydrothermal systems are explored in this study by applying reaction path modelling to the Ischia case study. Ischia Island, in Southern Italy, hosts a well-developed and structurally complex hydrothermal system which, because of its heterogeneity in chemical and physical properties, is an ideal test sites for evaluating potentialities/limitations of quantitative geochemical models of hydrothermal reactions. We used the EQ3/6 software package, version 7.2b, to model reaction of infiltrating waters (mixtures of meteoric water and seawater in variable proportions) with Ischia’s reservoir rocks (the Mount Ep…

010504 meteorology & atmospheric sciencesGeochemistryMineralogyengineering.material010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationHydrothermal systemGeochemistry and PetrologyMount Epomeo Green TuffPlagioclaseHydrothermal fluidIschia Island Reaction path modelling EQ3/60105 earth and related environmental sciencesMineralSettore GEO/08 - Geochimica E Vulcanologia13. Climate actionMeteoric waterengineeringPhenocrystSeawaterIschiaSaturation (chemistry)Clay mineralsGeologyGeochimica et Cosmochimica Acta
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Carbon isotope composition of CO2-rich inclusions in cumulate-forming mantle minerals from Stromboli volcano (Italy)

2017

We report on measurements of concentration and carbon isotope composition (δ13CCO2) of CO2 trapped in fluid inclusions of olivine and clinopyroxene crystals separated from San Bartolo ultramafic cumulate Xenoliths (SBX) formed at mantle depth (i.e., beneath a shallow Moho supposed to be at 14.8 km). These cumulates, erupted about 2 ka ago at Stromboli volcano (Italy), have been already investigated by Martelli et al. (2014) mainly for Sr-Nd isotopes and for their noble gases geochemistry. The concentration of CO2 varies of one order of magnitude from 3.8·10− 8 mol g− 1 to 4.8·10− 7 mol g− 1, with δ13C values between − 2.8‰ and − 1.5‰ vs V-PDB. These values overlap the range of measurements …

010504 meteorology & atmospheric sciencesGeochemistryUltramafic cumulateengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)Impact craterUltramafic rockGeochemistry and PetrologyFluid inclusionsXenolith0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryOlivineδ13CSettore GEO/07 - Petrologia E PetrografiaStromboli volcanoFluid inclusionGeophysicsVolcanoengineeringδ13CCO2MantleGeology
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Active Degassing of Deeply Sourced Fluids in Central Europe: New Evidences From a Geochemical Study in Serbia

2021

We report on the results of an extensive geochemical survey of fluids released in the Vardar zone (central-western Serbia), a mega-suture zone at the boundary between Eurasia and Africa plates. Thirty-one bubbling gas samples are investigated for their chemical and isotopic compositions (He, C, Ar) and cluster into three distinct groups (CO2-dominated, N2-dominated, and CH4-dominated) based on the dominant gas species. The measured He isotope ratios range from 0.08 to 1.19 Ra (where Ra is the atmospheric ratio), and reveal for the first time the presence of a minor (<20%) but detectable regional mantle-derived component in Serbia. δ13C values range from −20.2‰ to −0.1‰ (versus PDB), with…

010504 meteorology & atmospheric sciencesGeochemistrycarbon dioxidecarbon central Europe deep fluids fractionation helium mantlehelium010502 geochemistry & geophysics01 natural sciencesMantle (geology)chemistry.chemical_compoundGeophysicschemistrydeep fluidsGeochemistry and PetrologyCarbon dioxidecentral EuropefractionationGeologymantle0105 earth and related environmental sciences
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Geochemistry of Noble Gases and CO2 in Fluid Inclusions From Lithospheric Mantle Beneath Wilcza Góra (Lower Silesia, Southwest Poland)

2018

Knowledge of the products originating from the subcontinental lithospheric mantle (SCLM) is crucial for constraining the geochemical features and evolution of the mantle. This study investigated the chemistry and isotope composition (noble gases and CO2 ) of fluid inclusions (FI) from selected mantle xenoliths originating from Wilcza Góra (Lower Silesia, southwest Poland), with the aim of integrating their petrography and mineral chemistry. Mantle xenoliths are mostly harzburgites and sometimes bear amphiboles, and are brought to the surface by intraplate alkaline basalts that erupted outside the north-easternmost part of the Eger (Ohře) Rift in Lower Silesia. Olivine (Ol) is classified int…

010504 meteorology & atmospheric sciencesGeochemistryengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)chemistry.chemical_compoundNoble gasenoble gases CO2 fluid inclusions mantle xenoliths European mantle SCLM MORB metasomatismFluid inclusionsMetasomatismlcsh:ScienceAmphibole0105 earth and related environmental sciencesBasaltEuropean mantleOlivineSCLMmetasomatismPartial meltingAmbientaleFluid inclusionMORBMantle xenolithSilicatemantle xenolithsfluid inclusionschemistrynoble gasesengineeringGeneral Earth and Planetary Scienceslcsh:QCO2Geology
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Development of branching brittle and ductile shear zones: A numerical study

2017

Continental collision zones are usually associated with large-scale strike-slip shear zones. In most cases these shear zones are complex and consist of multiple strands, varying in width, length, and total displacement. Here we present 2-D numerical models to simulate the formation of such shear zones at different depth levels within the crust, under either brittle (frictional/plastic) or ductile conditions. Localization of shear zones is initiated by a material contrast (heterogeneity) of the material parameters. We systematically test the rate of strain-weakening in brittle and in ductile regimes to understand its influence on the development of shear zone networks. Our simulations sugges…

010504 meteorology & atmospheric sciencesGeometry010502 geochemistry & geophysics01 natural sciencesCondensed Matter::Soft Condensed MatterPhysics::Fluid DynamicsShear rateSimple shearStress fieldGeophysicsBrittlenessShear (geology)Geochemistry and PetrologyCritical resolved shear stressShear stressGeotechnical engineeringShear zoneGeology0105 earth and related environmental sciencesGeochemistry, Geophysics, Geosystems
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Collapse of a two-dimensional brittle granular column: Implications for understanding dynamic rock fragmentation in a landslide

2015

We investigate numerically the failure, collapse and flow of a two-dimensional brittle granular column over a horizontal surface. In our discrete element simulations, we consider a vertical monolayer of spherical particles that are initially held together by tensile bonds, which can be irreversibly broken during the collapse. This leads to dynamic fragmentation within the material during the flow. Compared to what happens in the case of a non-cohesive granular column, the deposit is much rougher, and the internal stratigraphic structure of the column is not preserved during the collapse. As has been observed in natural rockslides, we find that the deposit consists of large blocks laying on …

010504 meteorology & atmospheric sciencesGeometryLandslideRockslide01 natural sciences010305 fluids & plasmasEarth surfaceGeophysicsBrittlenessFragmentation (mass spectrometry)0103 physical sciencesMonolayerUltimate tensile strengthGeotechnical engineeringGeology0105 earth and related environmental sciencesEarth-Surface ProcessesJournal of Geophysical Research: Earth Surface
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Channel forms recovery in an ephemeral river after gravel mining (Palancia River, Eastern Spain)

2017

[EN] During the 1970s, the Palancia River was intensively affected by gravel mining instream. This activity completely destroyed the fluvial forms, devastating the original wandering pattern. At the end of the 1980s, gravel mining ceased and the river started a process of recovery, only altered by several clearing operations. The aim of this work is to describe these processes of change, analyzing the river's morphosedimentary conditions through a GIS analysis of aerial photographs previous to, simultaneous with, and subsequent to the intense gravel mining activity. Results explain the current difficulties of some ephemeral rivers to recover their original forms, because of the sediment and…

010504 meteorology & atmospheric sciencesHidrologiaFluvial010502 geochemistry & geophysics01 natural sciencesEphemeral riversSedimentsRiver trajectoriesClearing0105 earth and related environmental sciencesEarth-Surface ProcessesHydrologygeographygeography.geographical_feature_categoryLand useEphemeral keySedimentIncisionChannelizedCurrent (stream)Gravel miningLand use changesChannel (geography)GeologyChannel forms
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