Search results for "ATM"

showing 10 items of 24032 documents

Quartz grains reveal sedimentary palaeoenvironment and past storm events: A case study from eastern Baltic

2018

Abstract Sediment record collected from the coastal lake serves as a powerful tool for reconstructing changes in palaeoenvironment and understanding the potential signals of past storminess. In this study, we use several proxies from sediment of the Holocene Thermal Maximum at coastal Lake Lilaste, Latvia. We focus on surface texture of quartz grains from the mineral inorganic fraction as indicators of depositional environments. We then use this as a proxy for potential storm transport and combine with information on granulometry, diatom stratigraphy and chronology to answer the question whether flux of quartz grains in the lake originated from the sea or from the land. Analyses in a binocu…

010504 meteorology & atmospheric sciencesGeochemistryStormAquatic Science010502 geochemistry & geophysicsOceanography01 natural sciencesSedimentary depositional environment13. Climate actionGranulometryAeolian processesSedimentary rock14. Life underwaterGeomorphologyQuartzHoloceneGeology0105 earth and related environmental sciencesChronologyEstuarine, Coastal and Shelf Science
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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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Melt inclusions track melt evolution and degassing of Etnean magmas in the last 15 ka

2019

We present major elements compositions and volatiles contents of olivine-hosted melt inclusions from Etna volcano (Italy), which extend the existing database with the aim of interpreting the chemical variability of Etnean magmas over the last 15 ka. Olivine phenocrysts were selected from the most primitive Fall Stratified (FS) eruptive products of picritic composition (Mg# = 67–70, Fo 89–91 ), the Mt. Spagnolo eccentric lavas (Mg# = 52–64, Fo 82–88 ) and among the more recent 2002–2013 eruptive products (Mg# = 33–53, Fo 68–83 ). Crystal fractionation and degassing processes were modeled at temperatures of 1050–1300 °C, pressures <500 MPa, and oxygen fugacity between 1 and 2 log units abo…

010504 meteorology & atmospheric sciencesGeochemistryVolatile contentengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)Mineral redox bufferDegassingGeochemistry and PetrologySilicate melt inclusionPlagioclase0105 earth and related environmental sciencesMelt inclusionsFractional crystallization (geology)OlivineSpinelMelt differentiationGeologyEtna Silicate melt inclusions Volatile contents Melt differentiation Degassing13. Climate action[SDU]Sciences of the Universe [physics]engineeringPhenocrystEtnaGeology
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Rare earths behaviour during the deposition of volcanic sublimates

2017

Abstract In this study, the REE distribution between volcanic fluids and related solids in fumaroles with temperatures ranging from approximately 100 to 421 °C was investigated in different geological scenarios. The treatment of geochemical REE data was carried out by calculating the REE enrichment factors (EF REE ) relative to the volcanic host rocks in studied sites under the assumption that the REE transport takes place as silicate aerosol in volcanic fluids. Shale-normalised REE concentrations in these fluids have been assessed to investigate whether the REE transport as aqueous complexes in water-saturated volcanic gas is reasonable. The REE behaviour in alkaline condensates according …

010504 meteorology & atmospheric sciencesGeochemistryVolcanic condensatesSublimate010502 geochemistry & geophysicsVolcanic condensate01 natural sciencesAnthropogenic pollutionchemistry.chemical_compoundGd anomalyGeochemistry and PetrologySublimatesGeophysic0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryVolcanic islandsREESilicateFumaroleAerosolGeophysicsDeposition (aerosol physics)chemistryVolcanoVolcanic island[SDU]Sciences of the Universe [physics]Geology
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Comment on “Evolution of high-pressure mafic granulites and pelitic gneisses from NE Madagascar: Tectonic implications”. Tectonophysics, 662, 219–242…

2017

Abstract Determining the possible tectonic regimes active during the Neoproterozoic is crucial for the knowledge of the evolution of the super-continent Gondwana. In Madagascar, that occupies a key position in Gondwana, there is an on-going debate regarding the location of possible suture zones and the implications in terms of paleo-geography. Recognizing high-pressure to ultra-high pressure conditions in mafic rocks is commonly viewed as a strong argument for paleo-subduction zones. Ishwar-Kumar et al. (2015) report unusual high pressure conditions (24 kbar) in Neoproterozoic to Cambrian rocks from North-Central Madagascar (Andriamena Complex). They propose a geodynamic model in which exhu…

010504 meteorology & atmospheric sciencesGeochemistry[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/Petrography010502 geochemistry & geophysicsGranulite01 natural sciencesGondwanaGeophysics13. Climate actionFacies14. Life underwaterSuture (geology)MaficMetamorphic faciesGeologyComputingMilieux_MISCELLANEOUS[ SDU.STU.PE ] Sciences of the Universe [physics]/Earth Sciences/Petrography0105 earth and related environmental sciencesEarth-Surface ProcessesTerraneGneiss
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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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The impact of degassing on the oxidation state of basaltic magmas: A case study of Kīlauea volcano

2016

Volcanic emissions link the oxidation state of the Earth's mantle to the composition of the atmosphere. Whether the oxidation state of an ascending magma follows a redox buffer – hence preserving mantle conditions – or deviates as a consequence of degassing remains under debate. Thus, further progress is required before erupted basalts can be used to infer the redox state of the upper mantle or the composition of their co-emitted gases to the atmosphere. Here we present the results of X-ray absorption near-edge structure (XANES) spectroscopy at the iron K-edge carried out for a series of melt inclusions and matrix glasses from ejecta associated with three eruptions of Kīlauea volcano (Hawai…

010504 meteorology & atmospheric sciencesGeochemistrysub-05010502 geochemistry & geophysicsmelt inclusions01 natural sciencesMantle (geology)Mineral redox bufferOxidation stateGeochemistry and PetrologyHotspot (geology)Earth and Planetary Sciences (miscellaneous)EjectaGeophysic0105 earth and related environmental sciencesMelt inclusionsBasaltgeographygeography.geographical_feature_categorymelt inclusiondegassingoxygen fugacityXANESGeophysicsVolcanoSpace and Planetary SciencesulfurCO2Geology
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Extensive, water-rich magma reservoir beneath southern Montserrat

2016

South Soufriere Hills and Soufriere Hills volcanoes are two km apart at the southern end of the island of Montserrat, West Indies. Their magmas are distinct geochemically, despite these volcanoes having been active contemporaneously at 131-129 ka. We use the water content of pyroxenes and melt inclusion data to reconstruct the bulk water contents of magmas and their depth of storage prior to eruption. Pyroxenes contain up to 281 ppm H2O, with significant variability between crystals and from core to rim in individual crystals. The Al content of the enstatites from Soufriere Hills Volcano (SHV) is used to constrain melt-pyroxene partitioning for H2O. The SHV enstatite cores record melt water…

010504 meteorology & atmospheric sciencesGeochemistrysub-05Pyroxeneengineering.material010502 geochemistry & geophysics01 natural sciencesMushGeochemistry and PetrologyPlagioclase0105 earth and related environmental sciencesMelt inclusionsBasaltgeographygeography.geographical_feature_categoryAndesiteWaterGeologyAndesiteVolcano13. Climate actionMagmaengineeringInclusion (mineral)Melt inclusionsSIMSGeologyPyroxenes
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Causas y consecuencias del crecimiento urbanístico en el litoral valenciano a través de la evolución de los usos del suelo. El caso de Oliva.

2019

Mediante la fotointerpretación de imágenes aéreas con la utilización de técnicas SIG y a través de un intenso trabajo bibliográfico y de campo, se realiza un análisis diacrónico (1956, 1991 y 2015) de la evolución de los usos del suelo en Oliva (València, España). A partir de este análisis multimetodológico se estudia la evolución de la situación urbanística y de las dinámicas territoriales en un municipio paradigmático para explicar la evolución urbanística del litoral valenciano en las últimas décadas. In this paper we have carried out a diachronic analysis about land uses evolution in Olive through a mixed method of research, based on photo-interpretation of aerial images (years 1956, 19…

010504 meteorology & atmospheric sciencesGeography Planning and Development0211 other engineering and technologies02 engineering and technology01 natural sciencesValencianlanguage.human_languageGeographyDiachronic analysisTourism Leisure and Hospitality ManagementlanguageHumanities021101 geological & geomatics engineering0105 earth and related environmental sciencesNature and Landscape ConservationCuadernos de Turismo
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