Search results for "Geophysics"

showing 10 items of 2645 documents

The role of melt composition on aqueous fluid vs. silicate melt partitioning of bromine in magmas

2018

International audience; Volcanogenic halogens, in particular bromine, potentially play an important role in the ozone depletion of the atmosphere. Understanding bromine behaviour in magmas is therefore crucial to properly evaluate the contribution of volcanic eruptions to atmospheric chemistry and their environmental impact. To date, bromine partitioning between silicate melts and the gas phase is very poorly constrained, with the only relevant experimental studies limited to investigation of synthetic melt with silicic compositions. In this study, fluid/melt partitioning experiments were performed using natural silicate glasses with mafic, intermediate and silicic compositions. For each co…

atmospheric chemistry010504 meteorology & atmospheric sciencesbromine[SDU.STU]Sciences of the Universe [physics]/Earth SciencesSilicicarc magma010502 geochemistry & geophysics01 natural sciencesfluid/melt partitioningVolcanic Gaseschemistry.chemical_compoundGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)eventPetrologyGeophysic0105 earth and related environmental sciencesMelt inclusionsevent.disaster_typeBasaltAndesiteSettore GEO/07 - Petrologia E PetrografiadegassingSilicatearc magmasSettore GEO/08 - Geochimica E VulcanologiaGeophysicschemistry13. Climate actionSpace and Planetary ScienceMagmaMaficGeology
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Experimental Crystallization of a High-K Arc Basalt: the Golden Pumice, Stromboli Volcano (Italy)

2006

International audience; The near-liquidus crystallization of a high-K basalt (PST-9 golden pumice, 49·4 wt % SiO2, 1·85 wt % K2O, 7·96 wt % MgO) from the present-day activity of Stromboli (Aeolian Islands, Italy) has been experimentally investigated between 1050 and 1175°C, at pressures from 50 to 400 MPa, for melt H2O concentrations between 1·2 and 5·5 wt % and {Delta}NNO ranging from –0·07 to +2·32. A drop-quench device was systematically used. AuPd alloys were used as containers in most cases, resulting in an average Fe loss of 13% for the 34 charges studied. Major crystallizing phases include clinopyroxene, olivine and plagioclase. Fe–Ti oxide was encountered in a few charges. Clinopyro…

basalt010504 meteorology & atmospheric sciencesMineralogyLiquidusengineering.material010502 geochemistry & geophysics01 natural scienceslaw.inventionGeochemistry and Petrologylaw[SDE.MCG.CG]Environmental Sciences/Global Changes/domain_sde.mcg.cgPhase (matter)Pumicepumice[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanologyphase equilibriaPlagioclaseStrombolibasalt; pumice; experiment; phase equilibria; StromboliCrystallization0105 earth and related environmental sciencesBasaltOlivineexperimentSettore GEO/07 - Petrologia E PetrografiaGeophysicsengineeringInclusion (mineral)Geology
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Coseismic extension recorded within the damage zone of the Vado di Ferruccio Thrust Fault, Central Apennines, Italy

2018

Recent high resolution hypocentral localisation along active fault systems in the Central Apennines illuminates the activation of seismogenic volumes dipping at low angle (<30°) in extensional settings overprinting contractional deformations affecting the continental crust of the Adria microplate. Individuation of the geological structures and of the fault processes associated with these seismic patterns will contribute to the interpretation of seismic sequence evolution, and seismic hazard studies.Here we report field and microstructural evidence of seismogenic extensional faults localized within pre-existing thrust fault zones. The Vado di Ferruccio Thrust Fault (VFTF) is a narrow …

bepress|Physical Sciences and Mathematics010504 meteorology & atmospheric sciencesbepress|Physical Sciences and Mathematics|Earth Sciences|Tectonics and StructureWindow (geology)bepress|Physical Sciences and Mathematics|Earth SciencesActive faultFault (geology)EarthArXiv|Physical Sciences and Mathematics|Earth Sciences010502 geochemistry & geophysics01 natural sciencesFaults. Earthquakesbepress|Physical Sciences and Mathematics|Earth Sciences|Geophysics and SeismologyThrust fault0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryEarthArXiv|Physical Sciences and Mathematics|Earth Sciences|GeologyContinental crustbepress|Physical Sciences and Mathematics|Earth Sciences|GeologyGeologyOverprintingEarthArXiv|Physical Sciences and MathematicsTectonicsSeismic hazardGeology Faults. EarthquakesEarthArXiv|Physical Sciences and Mathematics|Earth Sciences|Geophysics and SeismologyEarthArXiv|Physical Sciences and Mathematics|Earth Sciences|Tectonics and StructureSeismologyGeology
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Early Paleocene Paleoceanography and Export Productivity in the Chicxulub Crater

2021

The Chicxulub impact caused a crash in productivity in the world''s oceans which contributed to the extinction of ~75% of marine species. In the immediate aftermath of the extinction, export productivity was locally highly variable, with some sites, including the Chicxulub crater, recording elevated export production. The long-term transition back to more stable export productivity regimes has been poorly documented. Here, we present elemental abundances, foraminifer and calcareous nannoplankton assemblage counts, total organic carbon, and bulk carbonate carbon isotope data from the Chicxulub crater to reconstruct changes in export productivity during the first 3 Myr of the Paleocene. We sh…

bepress|Physical Sciences and Mathematics|Earth Sciences|Paleontologybepress|Physical Sciences and Mathematicsbepress|Physical Sciences and Mathematics|Earth Sciences|Sedimentology010506 paleontologyAtmospheric Science010504 meteorology & atmospheric sciencesbepress|Physical Sciences and Mathematics|Earth SciencesEarthArXiv|Physical Sciences and Mathematics|Earth Sciences010502 geochemistry & geophysicsOceanography01 natural sciencesForaminifera/dk/atira/pure/sustainabledevelopmentgoals/life_below_waterWater columnImpact craterPaleoceanographyPhytoplanktonPhotic zone14. Life underwaterSDG 14 - Life Below WaterEarthArXiv|Physical Sciences and Mathematics|Earth Sciences|Sedimentology0105 earth and related environmental sciencesbiologyTerrigenous sedimentPaleontologyEarthArXiv|Physical Sciences and Mathematics|Earth Sciences|Geochemistry15. Life on landEarthArXiv|Physical Sciences and Mathematics|Earth Sciences|Paleontologybiology.organism_classificationhumanitiesEarthArXiv|Physical Sciences and MathematicsOceanographyProductivity (ecology)13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyEnvironmental sciencebepress|Physical Sciences and Mathematics|Earth Sciences|Geochemistry
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Sclerochronology and geochemical variation in limpet shells (Patella vulgata): A new archive to reconstruct coastal sea surface temperature

2007

[1] Climate archives contained in shells of the European limpet, Patella vulgata, accumulated in archaeological deposits can potentially provide much needed information about Holocene environmental change in midlatitude coastal areas. Before reconstructing climate information preserved in these zooarchaeological records, we studied the controls on oxygen and carbon isotope ratios (δ18O and δ13C, respectively) in modern specimens. We tested the hypothesis that P. vulgata precipitates its shell in isotopic equilibrium with the ambient water by comparing δ18OSHELL with predicted values. Predicted δ18OSHELL was constructed using observed sea surface temperature (SST) records and the equilibrium…

biologyEnvironmental changeδ18OLimpetbiology.organism_classificationEquilibrium fractionationSea surface temperatureGeophysicsOceanographyGeochemistry and PetrologyIsotopes of carbonSclerochronologyPatella vulgataGeologyGeochemistry, Geophysics, Geosystems
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Radial cracks around α-quartz inclusions in almandine: Constraints on the metamorphic history of the Oman mountains

1993

Radiating tensional cracks around α-quartz inclusions in almandine have been observed in metapelite samples from the southeastern Saih Hatat tectonic window, northeastern Oman Mountains. These almandines show an inclusion-rich (glaucophane + epidote) and strongly deformed core with inclusions of different mineral phases. The rim of the same almandines is inclusion-poor and shows only quartz, apatite, zircon, rutile and BaAl phosphates as inclusions. Quartz and apatite inclusions in the rim are single crystals often surrounded by radial cracks. These radial cracks developed during uplift by the dilation of α-quartz (4–5 vol%) without a phase transformation. Subsequently, these cracks were fi…

biologyGlaucophaneMetamorphic rockMineralogyEpidoteengineering.materialbiology.organism_classificationPhengiteAlmandineAlbiteGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)engineeringQuartzGeologyZirconEarth and Planetary Science Letters
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Gravity-Driven Infiltration and Subsidence Phenomena in Posidonia oceanica Residues

2019

A simplified infiltration model for highly permeable porous media was introduced, assuming the matric potential gradient as negligible compared to the gravitational gradient. This model enabled us to determine the delay time, i.e., the time that the water front takes (from the beginning of rainfall) to reach the bottom of the highly permeable layer. Posidonia oceanica (Linnaeus) Delile residues were used as a porous media, in order to study the infiltration process that provides salt leaching under natural rainfall when these residues are arranged in a storage area, before reusing. By using a laboratory rainfall simulator, delay times were measured to verify the applicability of the aforeme…

biologyGravity-driven infiltrationPhysics::OpticsSoil sciencebiology.organism_classificationGravity gradientPhysics::GeophysicsInfiltration (hydrology)Water potentialPosidonia oceanicaPhysics::Space PhysicsEnvironmental ChemistryInfiltration delay timeSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliPorous mediumGeologyPosidonia oceanica residueGeneral Environmental ScienceWater Science and TechnologyCivil and Structural Engineering
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Climate change at the 4.2 ka BP termination of the Indus valley civilization and Holocene south Asian monsoon variability

2003

[1] Planktonic oxygen isotope ratios off the Indus delta reveal climate changes with a multi-centennial pacing during the last 6 ka, with the most prominent change recorded at 4.2 ka BP. Opposing isotopic trends across the northern Arabian Sea surface at that time indicate a reduction in Indus river discharge and suggest that later cycles also reflect variations in total annual rainfall over south Asia. The 4.2 ka event is coherent with the termination of urban Harappan civilization in the Indus valley. Thus, drought may have initiated southeastward habitat tracking within the Harappan cultural domain. The late Holocene drought cycles following the 4.2 ka BP event vary between 200 and 800 y…

biologyIndusClimate changebiology.organism_classificationMonsoonGeophysicsOceanographyPaleoclimatologyGeneral Earth and Planetary SciencesQuaternaryCenozoicGlobigerinoidesHoloceneGeologyGeophysical Research Letters
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Effect of organic matrices on the determination of the trace element chemistry (Mg, Sr, Mg/Ca, Sr/Ca) of aragonitic bivalve shells (<i>Arctica …

2010

The element chemistry of biogenic carbonates can provide important data on past environments. However, the Sr/Ca and Mg/Ca ratios as well as the Mg and Sr concentrations of biological carbonates, especially aragonitic bivalves often depart from apparent thermodynamic equilibrium. When measured in situ by means of LA-ICP-MS, the Mg concentration is often substantially enriched (two- to threefold) near the organic-rich, annual growth lines. To test the hypothesis that some organic components exert a major influence on the skeletal metal content, the element chemistry of different shell components (insoluble organic matrix, IOM; dissolved CaCO3 and soluble organics, SOM) of Arctica islandica w…

biologyMagnesiumTrace elementchemistry.chemical_elementCalciumbiology.organism_classificationMetalGeophysicschemistryGeochemistry and PetrologyInductively coupled plasma atomic emission spectroscopyEnvironmental chemistryvisual_artvisual_art.visual_art_mediumBivalve shellArctica islandicaChemical compositionGEOCHEMICAL JOURNAL
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Identification of metalloporphyrins extracted from the copper bearing black shale of fore sudetic monocline (Poland)

2006

Abstract Metalloporphyrins were isolated from copper-bearing black shale ores. The shale originates from the Lubin copper mine (Poland). The porphyrins have been extracted by way of a Soxhlet apparatus, and then purified using column chromatography. In order to identify the extracted porphyrins complexes UV–Vis, mass spectrometry and EPR analytical techniques have been used.

black shale oresChemistryMechanical EngineeringMineralogychemistry.chemical_elementGeneral Chemistry010501 environmental sciences010502 geochemistry & geophysicsGeotechnical Engineering and Engineering GeologyMass spectrometrygeoporphyrins extraction01 natural sciencesCoppermetalloporphyrins analytical studiesColumn chromatographyMonoclineControl and Systems Engineering[ CHIM.OTHE ] Chemical Sciences/Other[CHIM.OTHE]Chemical Sciences/OtherCopper mineOil shaleComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesNuclear chemistry
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