Search results for "Volcano"

showing 10 items of 591 documents

Simulation des sorties d'eau et de nitrates de parcelles agricoles drainées. Cas du site expérimental de Virey-le-Grand (71)

2003

[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology[SDE.MCG.CG] Environmental Sciences/Global Changes/domain_sde.mcg.cg[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics[SDU.STU.VO] Sciences of the Universe [physics]/Earth Sciences/Volcanology[ SDE.MCG.CG ] Environmental Sciences/Global Changes/domain_sde.mcg.cg[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/Tectonics[ SDU.STU.VO ] Sciences of the Universe [physics]/Earth Sciences/Volcanology[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/Climatology
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Signatures terrigène et volcanique des bassins sédimentaires : implications stratigraphiques et paléoclimatiques

2018

[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatologysédimentation des argilesstratigraphiepaleoclimate[SDU.STU.VO] Sciences of the Universe [physics]/Earth Sciences/Volcanologypaleoenvironmentspaléoclimat[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/Stratigraphystratigraphypaleovolcanismeclay sedimentationpaléoenvironnentspaléovolcanisme
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Phase equilibrium constraints on the production and storage of peralkaline silicic magmas: insights from Kenya and Pantelleria.

2005

The origin of peralkaline silicic rocks is still obscure and stands perhaps as one of the last major unsettled issues in classic igneous petrology. The debate goes back to the end of the 18th century and despite intensive petrological, geochemical and laboratory efforts the consensus has yet to emerge as to which mechanisms produce peralkaline derivatives. Bowen (1937) first proposed that the shift from metaluminous to peralkaline field was due to extensive fractionation of calcic plagioclase. Perhaps the best illustration of such an hypothesis is provided by the Boina rock series in the Ethiopian rift studied by Barberi et al. (1975). However, such an hypothesis still awaits experimental c…

[SDU.STU.VO] Sciences of the Universe [physics]/Earth Sciences/Volcanology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology
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In-situ characterisation of aerosol and gases (SO 2 , HCl, ozone) in Mt Etna volcano plume

2015

International audience; We present findings from a measurement campaign that deployed a range of in-situ real-time atmospheric measurement techniques to characterise aerosols and gases in Mt Etna plume in October 2013. The LOAC (Light Optical Aerosol Counter) instrument for size-resolved particle measurements was deployed alongside two Multi-Gas instruments (measuring SO 2 , H2S, HCl, CO 2) and an ozone sensor. Measurements were performed at the summit craters (in cloudy-and non-cloudy conditions) and in grounding downwind plume on the volcano flank. These high frequency measurements (acid gases: 1 to 0.1 Hz, aerosol: 0.1 Hz) provide a detailed in-situ dataset for time-resolved plume charac…

[SDU] Sciences of the Universe [physics][SDU]Sciences of the Universe [physics][SDU.STU.VO] Sciences of the Universe [physics]/Earth Sciences/Volcanology[SDU.STU] Sciences of the Universe [physics]/Earth Sciences[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
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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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Magma and volatile supply to post-collapse volcanism and block resurgence in Siwi caldera (Tanna Island, Vanuatu arc)

2011

Siwi caldera, in the Vanuatu arc (Tanna island), is a rare volcanic complex where both persistent eruptive activity (Yasur volcano) and rapid block resurgence (Yenkahe horst) can be investigated simultaneously during a post-caldera stage. Here we provide new constraints on the feeding system of this volcanic complex, based on a detailed study of the petrology, geochemistry and volatile content of Yasur-Siwi bulk-rocks and melt inclusions, combined with measurements of the chemical composition and mass fluxes of Yasur volcanic gases. Major and trace element analyses of Yasur-Siwi volcanic rocks, together with literature data for other volcanic centers, point to a single magmatic series and p…

blockEarth scienceAndesiteYasur magmatic degassingvolcano thermal budgetVanuatu arcGeochemistryPyroclastic rockVolcanologyVolcanismmelt inclusionsBlock (meteorology)volatilesGeophysicsGeochemistry and PetrologyresurgentMagma[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyCalderagas fluxes[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentYasurGeologyMelt inclusions
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Geochemistry and petrography of box-core sediments from a methane seep setting in the Strait of Sicily, central Mediterranean

2008

box-core sediment mud volcano SE SicilySettore GEO/08 - Geochimica E Vulcanologia
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Molecular and isotopic composition of free hydrocarbon gases from Sicily, Italy

2004

[1] Chemical and isotopic data have been used as geochemical tracers for a genetic characterization of hydrocarbon gases from a total of eleven manifestations located in Eastern and Central-Southern Sicily (Italy). The molecular analysis shows that almost all the samples are enriched in methane (up to 93.2% Vol.), with the exception of four gas samples collected around Mt. Etna showing high mantle-derived CO2 content. Methane isotope signatures suggest that these are thermogenic gases or a mixture between thermogenic gases and microbial gases. Although samples from some mud volcanoes in Southern Sicily (Macalube di Aragona) show isotope signatures consistent with a mixing model between ther…

chemistry.chemical_classificationIsotopeMineralogyMethaneMantle (geology)chemistry.chemical_compoundGeophysicsHydrocarbonCO2 contentchemistryEnvironmental chemistryOrganic geochemistryGeneral Earth and Planetary SciencesDiel vertical migrationGeologyMud volcanoGeophysical Research Letters
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Tracing the source of gypsum in New Caledonian soils by REE contents and SSr isotopic compositions

1998

Gypsum minerals forming in pedogenic environments in New Caledonia were examined for their S and Sr isotope compositions and REE distributions. Three possible sources were identified: volcanic, soil-derived and marine. However, differentiation based only on the REE contents and normalized patterns was not possible, but, the best preserved volcanic sample yields a negative EuEu∗ anomaly and the lowest GdNYbN ratio due to the high content of organic matter. Mixing calculations of the δ34S values and 87Sr86Sr ratios confirmed that the marine gypsum has a δ34S value close to + 21‰ and an 87Sr86Sr ratio close to 0.70912, and that the volcanic gypsum has a δ34S value of 0‰ and an 87Sr86Sr ratio o…

chemistry.chemical_classificationgeographyGypsumgeography.geographical_feature_categoryGeochemistryMineralogyGeologyFractionationengineering.materialδ34SPedogenesischemistryVolcanoSource rockGeochemistry and PetrologySoil waterengineeringOrganic matterGeologyChemical Geology
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2017

Abstract. Remote sensing of the gaseous composition of non-eruptive, passively degassing volcanic plumes can be a tool to gain insight into volcano interior processes. Here, we report on a field study in September 2015 that demonstrates the feasibility of remotely measuring the volcanic enhancements of carbon dioxide (CO2), hydrogen fluoride (HF), hydrogen chloride (HCl), sulfur dioxide (SO2), and bromine monoxide (BrO) in the downwind plume of Mt. Etna using portable and rugged spectroscopic instrumentation. To this end, we operated the Fourier transform spectrometer EM27/SUN for the shortwave-infrared (SWIR) spectral range together with a co-mounted UV spectrometer on a mobile platform in…

event.disaster_typeAtmospheric Sciencegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesSpectrometer010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesPlumeVolcanic Gaseschemistry.chemical_compoundAltitudeImpact craterVolcanochemistrySunriseeventGeologySulfur dioxide0105 earth and related environmental sciencesRemote sensingAtmospheric Measurement Techniques
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