Search results for "Geophysic"

showing 10 items of 2684 documents

Environmental change during the Early Cretaceous in the Purbeck-type Durlston Bay section (Dorset, Southern England): a biomarker approach.

2007

20 pages; International audience; The Purbeck-type section (Durlston Bay, Dorset, UK) exhibits littoral lagoonal to lacustrine facies. It shows a gradual climatic/environmental change from semi-arid conditions associated with evaporites at the Jurassic–Cretaceous transition, to a more humid climate at the end of the Berriasian. Though generally organic-poor (total organic carbon, TOC, <1.3%), the Durlston Bay section shows an organic-rich episode (TOC up to 8.5%) located at the transition from evaporitic to more humid facies. A biomarker study was performed in order to determine the origin of the organic matter (OM) in the section and see if changes in organic sources accompanied the genera…

010504 meteorology & atmospheric sciencesEnvironmental change[SDE.MCG]Environmental Sciences/Global ChangesBotryococcus010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciences[ SDE.MCG.CPE ] Environmental Sciences/Global Changes/domain_sde.mcg.cpeBottom waterSteranechemistry.chemical_compoundGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry0105 earth and related environmental sciencesTotal organic carbonbiologyEcology15. Life on landbiology.organism_classification[SDE.MCG.CPE]Environmental Sciences/Global Changes/domain_sde.mcg.cpe[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry6. Clean waterCretaceousPalynofacies[ SDE.MCG ] Environmental Sciences/Global Changeschemistry13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyBayGeology
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Impact of basin burial and exhumation on Jurassic carbonates diagenesis on both sides of a thick clay barrier (Paris Basin, NE France).

2014

27 pages; International audience; Several diagenetic models have been proposed for Middle and Upper Jurassic carbonates of the eastern Paris Basin. The paragenetic sequences are compared in both aquifers to propose a diagenetic model for the Middle and Late Jurassic deposits as a whole. Petrographic (optical and cathodoluminescence microscopy), structural (fracture orientations) and geochemical (δ18O, δ13C, REE) studies were conducted to characterize diagenetic cements, with a focus on blocky calcite cements, and their connection with fracturation events. Four generations of blocky calcite (Cal1-Cal4) are identified. Cal1 and Cal2 are widespread in the dominantly grain-supported facies of t…

010504 meteorology & atmospheric sciencesEvaporiteCarbonateStratigraphyGeochemistryJurassic[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysicsOceanography01 natural sciencesDiagenesisPetrographyOxygen and carbon isotopesPaleontologychemistry.chemical_compoundParis Basin[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/MineralogyRare earth elements0105 earth and related environmental sciencesCalciteGeologyCementation (geology)6. Clean waterCretaceousDiagenesisGeophysicschemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesEconomic GeologyPaleogeneGeology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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The behaviour of zirconium, hafnium and rare earth elements during the crystallisation of halite and other salt minerals

2017

Abstract Halite crystals from Messinian and Tortonian evaporites from Sicily and Spain and current precipitated halite crystals and the relative parent brines (active evaporation systems) were investigated in order to evaluate the Zr, Hf and Rare Earth Element (REE) behaviour. Halite crystallisation from evaporating brines fractionates Zr, Hf and REE through a two-step process. During the first step, dissolved complexes of studied elements are scavenged onto the surfaces of crystallising halite. During the second step, elements are co-precipitated into the crystal lattice as it grows. The first step mechanism is determined by the dissolved REE speciation. In saltworks where carbonate-REE co…

010504 meteorology & atmospheric sciencesEvaporiteGeochemistryMineralogychemistry.chemical_elementengineering.material010502 geochemistry & geophysics01 natural sciencesGeochemistry and PetrologySettore CHIM/01 - Chimica AnaliticaZr/HfDissolution0105 earth and related environmental sciencesZirconiumRare-earth elementGeologyAuthigenicHaliteREESettore GEO/08 - Geochimica E VulcanologiaDiagenesisEvaporitechemistryengineeringHaliteSeawaterGeologyChemical Geology
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Zr/Hf ratio and REE behaviour: A coupled indication of lithogenic input in marginal basins and deep-sea brines

2019

Abstract The distribution of dissolved Zr, Hf and Rare Earth Elements (yttrium and lanthanides, hereafter referred to as REE) in the Eastern Mediterranean seawater column was measured in the Kryos basin to evaluate the lithogenic contribution from both Nile River and Sahara and Arabian desert dust. We found dissolved Zr/Hf ratios below the signature of crustal rocks and chondrites; a phenomenon likely driven by the dissolution of the Mn-rich coating of atmospheric dust particles delivered from the desert. In deeper waters, Zr/Hf ratios are clustered close to the signature of crustal rocks and chondrites according to the different Zr and Hf dissolved speciation. The Zr/Hf ratio observed in t…

010504 meteorology & atmospheric sciencesEvaporiteGeochemistrychemistry.chemical_elementYttrium010502 geochemistry & geophysicsOceanography01 natural sciencesDeep seaAnoxic watersWaves and shallow waterOceanographychemistryChondriteSeawaterZr/HfDissolutionGeology0105 earth and related environmental sciencesDeep Sea Research Part II: Topical Studies in Oceanography
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Blast waves from violent explosive activity at Yasur Volcano, Vanuatu

2013

[1] Infrasonic and seismic waveforms were collected during violent strombolian activity at Yasur Volcano (Vanuatu). Averaging ~3000 seismic events showed stable waveforms, evidencing a low-frequency (0.1–0.3 Hz) signal preceding ~5–6 s the explosion. Infrasonic waveforms were mostly asymmetric with a sharp compressive (5–106 Pa) onset, followed by a small long-lasting rarefaction phase. Regardless of the pressure amplitude, the ratio between the positive and negative phases was constant. These waveform characteristics closely resembled blast waves. Infrared imagery showed an apparent cold spherical front ~20 m thick, which moved between 342 and 405 m/s before the explosive hot gas/fragments…

010504 meteorology & atmospheric sciencesExplosive materialFront (oceanography)RarefactionGeophysics010502 geochemistry & geophysics01 natural sciencesStrombolian eruptionsymbols.namesakeGeophysicsCold frontMach number13. Climate actionsymbolsGeneral Earth and Planetary SciencesSupersonic speedGeologyBlast waveSeismology0105 earth and related environmental sciencesGeophysical Research Letters
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Magma extrusion during the Ubinas 2013-2014 eruptive crisis based on satellite thermal imaging (MIROVA) and ground-based monitoring

2015

International audience; After 3 years of mild gases emissions, the Ubinas volcano entered in a new eruptive phase on September 2nd, 2013. The MIROVA system (a space-based volcanic hot-spot detection system), allowed us to detect in near real time the thermal emissions associated with the eruption and provided early evidence of magma extrusion within the deep summit crater. By combining IR data with plume height, sulfur emissions, hot spring temperatures and seismic activity, we interpret the thermal output detected over Ubinas in terms of extrusion rates associated to the eruption. We suggest that the 2013–2014 eruptive crisis can be subdivided into three main phases: (i) shallow magma intr…

010504 meteorology & atmospheric sciencesExplosive materialLava010502 geochemistry & geophysics01 natural sciencesImpact craterGeochemistry and PetrologyThermal[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyThermal anomalies0105 earth and related environmental sciencesHot springgeographygeography.geographical_feature_categoryExtrusion rates; earthquake; MIROVA; Thermal anomalies; Ubinas; Geochemistry and Petrology; GeophysicsMIROVAGeophysicsVolcano13. Climate actionUbinasearthquakeMagmaSatelliteExtrusion ratesSeismologyGeology
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Ground deformation reveals the scale-invariant conduit dynamics driving explosive basaltic eruptions

2021

The mild activity of basaltic volcanoes is punctuated by violent explosive eruptions that occur without obvious precursors. Modelling the source processes of these sudden blasts is challenging. Here, we use two decades of ground deformation (tilt) records from Stromboli volcano to shed light, with unprecedented detail, on the short-term (minute-scale) conduit processes that drive such violent volcanic eruptions. We find that explosive eruptions, with source parameters spanning seven orders of magnitude, all share a common pre-blast ground inflation trend. We explain this exponential inflation using a model in which pressure build-up is caused by the rapid expansion of volatile-rich magma ri…

010504 meteorology & atmospheric sciencesExplosive materialScienceGeneral Physics and AstronomyMagnitude (mathematics)VolcanologyDeformation (meteorology)010502 geochemistry & geophysics01 natural sciencestiltGeneral Biochemistry Genetics and Molecular BiologyArticlePhysics::Geophysicsground deformationElectrical conduitOrders of magnitude (specific energy)ground deformation conduit dynamics early warningAstrophysics::Solar and Stellar AstrophysicsStromboli0105 earth and related environmental sciencesgeographyMultidisciplinarygeography.geographical_feature_categoryExplosive eruptionQGeneral ChemistryGeophysicsVolcanoMagmaSeismologyGeologyNature Communications
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Geophysical prospection of the Roman city of Pollentia, Alcúdia (Mallorca, Balearic Islands, Spain)

2016

Abstract We present the results of the geophysical investigation carried out in the Roman city of Pollentia, in the island of Mallorca. The ancient city was identified in the 19th century. Old and new archaeological excavations have helped to uncover a residential area, a theatre, the forum, several necropolises and other remains of the city, but a large unexplored area has still to be investigated. For instance, the limits of the ancient town and the presence of harbour structures are still unknown. The geophysical survey has covered an area of more than 20.000 m2 by integrating magnetic, electromagnetic, electrical and ground penetrating radar (GPR) methods. Many unseen archaeological fea…

010504 meteorology & atmospheric sciencesGPRMagneticgovernment.political_district010502 geochemistry & geophysics01 natural sciencesSettore GEO/11 - Geofisica ApplicataElectrical resistivity tomographyElectrical resistivity tomographyArchaeological prospection0105 earth and related environmental sciencescomputer.programming_languagegeographyBalearic islandsgeography.geographical_feature_categoryEM surveyExcavationcomputer.file_formatArchaeologyResidential areaGeophysicsPollentiaGeophysical survey (archaeology)VRMLHarbourGround-penetrating radargovernmentArchaeological prospection; Electrical resistivity tomography; EM survey; GPR; Magnetic; Pollentia; GeophysicscomputerJournal of Applied Geophysics
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On the timing between terrestrial gamma ray flashes, radio atmospherics, and optical lightning emission

2017

On 25 October 2012 the Reuven Ramaty High Energy Solar Spectroscope Imager (RHESSI) and the Tropical Rainfall Measuring Mission (TRMM) satellites passed over a thunderstorm on the coast of Sri Lanka. RHESSI observed a terrestrial gamma ray flash (TGF) originating from this thunderstorm. Optical measurements of the causative lightning stroke were made by the lightning imaging sensor (LIS) on board TRMM. The World Wide Lightning Location Network (WWLLN) detected the very low frequency (VLF) radio emissions from the lightning stroke. The geolocation from WWLLN, which we also assume is the TGF source location, was in the convective core of the cloud. By using new information about both RHESSI a…

010504 meteorology & atmospheric sciencesGamma rayFOS: Physical sciencesRadio atmosphericLight curve01 natural sciencesLightningSpace Physics (physics.space-ph)GeophysicsPhysics - Space PhysicsSpace and Planetary Science0103 physical sciencesThunderstormEnvironmental scienceAtmosphericsVery low frequencyAstrophysics - Instrumentation and Methods for AstrophysicsInstrumentation and Methods for Astrophysics (astro-ph.IM)010303 astronomy & astrophysics0105 earth and related environmental sciencesTerrestrial gamma-ray flashRemote sensingJournal of Geophysical Research: Space Physics
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Enhanced detection of terrestrial gamma-ray flashes by AGILE

2015

At the end of March 2015 the onboard software configuration of the Astrorivelatore Gamma a Immagini Leggero (AGILE) satellite was modified in order to disable the veto signal of the anticoincidence shield for the minicalorimeter instrument. The motivation for such a change was the understanding that the dead time induced by the anticoincidence prevented the detection of a large fraction of Terrestrial Gamma-Ray Flashes (TGFs). The configuration change was highly successful resulting in an increase of one order of magnitude in TGF detection rate. As expected, the largest fraction of the new events has short duration (<100 μs), and part of them has simultaneous association with lightning sfer…

010504 meteorology & atmospheric sciencesGamma rayRadio atmosphericDead time01 natural sciencesLightningWorld wideGeophysics13. Climate action0103 physical sciencesGeneral Earth and Planetary SciencesEnvironmental scienceSatelliteAtmospheric electricity010303 astronomy & astrophysicsShort duration0105 earth and related environmental sciencesRemote sensingGeophysical Research Letters
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