Search results for "volcan"

showing 10 items of 899 documents

First in-situ measurements of plume chemistry at mount garet volcano, island of gaua (Vanuatu)

2020

Recent volcanic gas compilations have urged the need to expand in-situ plume measurements to poorly studied, remote volcanic regions. Despite being recognized as one of the main volcanic epicenters on the planet, the Vanuatu arc remains poorly characterized for its subaerial emissions and their chemical imprints. Here, we report on the first plume chemistry data for Mount Garet, on the island of Gaua, one of the few persistent volatile emitters along the Vanuatu arc. Data were collected with a multi-component gas analyzer system (multi-GAS) during a field campaign in December 2018. The average volcanic gas chemistry is characterized by mean molar CO2/SO2, H2O/SO2, H2S/SO2 and H2/SO2 ratios …

010504 meteorology & atmospheric sciencesvolcanic gas compositionsGeochemistryFlux010502 geochemistry & geophysicslcsh:Technology01 natural scienceslcsh:ChemistryVanuatu[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyGeneral Materials ScienceGas composition[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentlcsh:QH301-705.5Instrumentation0105 earth and related environmental sciencesFluid Flow and Transfer Processesgeographygeography.geographical_feature_categorySubductionlcsh:TProcess Chemistry and TechnologyGeneral Engineeringlcsh:QC1-999Gas analyzerComputer Science ApplicationsPlumelcsh:Biology (General)lcsh:QD1-999Mount GaretVolcanolcsh:TA1-2040SubaerialPeriod (geology)volatile fluxeslcsh:Engineering (General). Civil engineering (General)GauaGaua Mount Garet Multi-GAS Vanuatu Volatile fluxes Volcanic gas compositionslcsh:PhysicsMulti-GAS
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Mercury emissions from soils and fumaroles of Nea Kameni volcanic centre, Santorini (Greece)

2013

There have been limited studies to date targeting mercury emissions from volcanic fumarolic systems, and no mercury flux data exist for soil or fumarolic emissions at Santorini volcanic complex, Greece. We present results from the first geochemical survey of Hg and major volatile (CO2, H2S, H2O and H-2) concentrations and fluxes in the fumarolic gases released by the volcanic/hydrothermal system of Nea Kameni islet; the active volcanic center of Santorini. These data were obtained using a portable mercury spectrometer (Lumex 915+) for gaseous elemental mercury (GEM) determination, and a Multi-component Gas Analyzer System (Multi-GAS) for major volatiles. Gaseous Elemental Mercury (GEM) conc…

010504 meteorology & atmospheric sciencesvolcanogenic mercury volcanic degassing Santorini mercury flux inventory trace metalsEarth sciencetrace metalsAir pollutionchemistry.chemical_element010502 geochemistry & geophysicsmedicine.disease_cause01 natural scienceschemistry.chemical_compoundGeochemistry and Petrologymercury flux inventorymedicinevolcanogenic mercuryAir quality index0105 earth and related environmental sciencesgeographySantorinigeography.geographical_feature_categoryFumaroleSettore GEO/08 - Geochimica E VulcanologiaMercury (element)GeophysicschemistryVolcano13. Climate actionEnvironmental chemistryCarbon dioxideSoil watervolcanic degassingGeologyGEOCHEMICAL JOURNAL
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Evidence of aerial volcanic activity during the Valanginian along the northern Tethys margin.

2009

7 pages; International audience; Stratigraphic measurement and sampling on three sections (Vergol, La Charce, and Montclus) through Valanginian deposits from the Vocontian Basin (southeastern France) reveals the occurrence of centimetre thick ochre-coloured layers, which can be correlated from one section to another. At least twelve of these are identified in sediments dated from the Pertransiens to Furcillata ammonite Zones. These horizons appear similar to previously described Oxfordian and Aptian bentonites, also from the Vocontian Basin. Clay-mineralogical and geochemical data are similar in the Valanginian ochre horizons and their enclosing marls except in one of these that shows a cla…

010506 paleontologyAptian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesBentonite.PaleontologyVolcanismPassive margin[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMarl[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/Mineralogy0105 earth and related environmental sciencesAmmoniteHorizon (geology)geographygeography.geographical_feature_categoryPaleontology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrylanguage.human_languageCretaceousVocontian BasinVolcano13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyValanginianlanguageBentoniteGeologyVolcanic ash[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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New Insights into the Provenance of the Obsidian Fragments of the Island of Ustica (Palermo, Sicily)

2016

In this study we applied a multidisciplinary approach, coupling geophysical and geochemical measurements, to unveil the provenance of 170 obsidian flakes, collected on the volcanic island of Ustica (Sicily). On this island there are some prehistoric settlements dated from the Neolithic to the Middle Bronze Age. Despite not having geological outcrops of obsidian rocks, the countryside of Ustica is rich in fragments of this volcanic glass, imported from other source areas. The study of obsidian findings was carried out first through visual observations and density measurements. At least two different obsidian families have been distinguished, probably imported from Lipari and Pantelleria isla…

010506 paleontologyArcheologyHistoryProvenance060102 archaeologyVolcanic islandOutcrop06 humanities and the arts01 natural sciencesArchaeologyVolcanic glassPrehistorychemistry.chemical_compoundchemistryBronze Age0601 history and archaeologyGeology0105 earth and related environmental sciencesEMPAArchaeometry
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Volcanic climate forcing preceding the inception of the Younger Dryas: Implications for tracing the Laacher See eruption

2021

Climatic warming from the last glacial maximum to the current interglacial period was punctuated by a similar to 1300 years long cold period, commonly referred to as the Younger Dryas (YD). Several hypotheses have been proposed for the mechanism triggering the abrupt inception of the YD, including freshwater forcing, an extra-terrestrial impact, and aerosols from volcanic eruptions. Here, we use synchronised sulphate and sulphur records from both Greenland and Antarctic ice cores to reconstruct volcanic forcing between 13,200-12,800 a BPGICC05 (years before 1950 CE on the Greenland Ice Core Chronology 2005; GICC05). This continuous reconstruction of stratospheric sulphur injections highligh…

010506 paleontologyArcheologyYounger Dryas010504 meteorology & atmospheric sciences530 PhysicsCIRCULATIONIce cores; Laacher See eruption; Sulphate; Volcanic radiative forcing; Younger DryasSULFURForcing (mathematics)01 natural sciencesVolcanic radiative forcingANTARCTIC ICE-CORESOCEANIce coreCHRONOLOGYYounger Dryas550 Earth sciences & geologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary Changegeographygeography.geographical_feature_categoryGeologyLast Glacial MaximumRECORDWAIS DIVIDESulphateRadiative forcingGREENLANDLaacher See eruptionVolcano13. Climate actionIce coresClimatologySYNCHRONIZATIONInterglacialClimate modelSULFATEGeologyQuaternary Science Reviews
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The first archaeometric characterization of obsidian artifacts from the archaeological site of Samshvilde (South Georgia, Caucasus)

2019

This paper presents the first results about the provenance of obsidian fragments recovered in the archaeological site of Samshvilde (South Georgia, Caucasus) with the aim to obtain knowledge related to the network distribution and procurement of obsidian in Georgia. The geochemical characterization of thirty archaeological finds was obtained by the LA-ICP-MS method, an almost non-destructive technique capable of chemically characterizing the volcanic glass. A comparison of geochemical results obtained on both archaeological artefacts and geological samples collected from Chikiani outcrop in Georgia, together with literature data of southern Caucasus and eastern Turkey, allowed us to define …

010506 paleontologyArcheologygeographyProvenancegeography.geographical_feature_category060102 archaeologyOutcrop06 humanities and the arts01 natural sciencesArchaeologyVolcanic glassObsidian Trace elements LA-ICP-MS Samshvilde GeorgiaVolcanoAnthropology0601 history and archaeologySettore GEO/09 -Georis. Miner.e Appl.Mineral.-Petrogr. per l'Ambi.ed i B.Cult.Geology0105 earth and related environmental sciencesArchaeological and Anthropological Sciences
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The ELSA tephra stack: Volcanic activity in the Eifel during the last 500,000 years

2016

Abstract Tephra layers of individual volcanic eruptions are traced in several cores from Eifel maar lakes, drilled between 1998 and 2014 by the Eifel Laminated Sediment Archive (ELSA). All sediment cores are dated by 14C and tuned to the Greenland interstadial succession. Tephra layers were characterized by the petrographic composition of basement rock fragments, glass shards and characteristic volcanic minerals. 10 marker tephra, including the well-established Laacher See Tephra and Dumpelmaar Tephra can be identified in the cores spanning the last glacial cycle. Older cores down to the beginning of the Elsterian, show numerous tephra sourced from Strombolian and phreatomagmatic eruptions,…

010506 paleontologyGlobal and Planetary Changegeographygeography.geographical_feature_categoryEarth scienceGeochemistry010502 geochemistry & geophysicsOceanography01 natural sciencesLapilliStrombolian eruptionMaarVolcanoMagmaPhreatomagmatic eruptionTephraTephrochronologyGeology0105 earth and related environmental sciencesGlobal and Planetary Change
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The metamorphic rocks of the Nunatak Viedma in the Southern Patagonian Andes: Provenance sources and implications for the early Mesozoic Patagonia-An…

2019

The Nunatak Viedma within the Southern Patagonian Icefield has been considered as a volcanic center based on its geomorphologic features, despite the fact that field explorations by Eric Shipton determined its metamorphic nature 70 years ago. We carried out fieldwork to characterize this isolated outcrop and performed the first U-Pb dating in detrital zircons from the basement rocks located inside the Southern Patagonian Icefield. We recognized very-low grade metamorphic rocks, corresponding principally to metapelites and metapsammites, and scarce metabasites. Detrital zircons in three metapsammitic samples (composite group of 240 grains) yielded prominent age population peaks at ∼1090, ∼96…

010506 paleontologyProvenanceNunatakVery-low grade metamorphic rocksOutcropMetamorphic rockPopulationDetrital zircons agesDETRITAL ZIRCONS AGES[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysics01 natural sciencesSouthwestern GondwanaCiencias de la Tierra y relacionadas con el Medio Ambiente//purl.org/becyt/ford/1 [https]Southern Patagonian Andes//purl.org/becyt/ford/1.5 [https]PaleontologyAntarctic PeninsulaCarboniferousGeologíaVERY-LOW GRADE METAMORPHIC ROCKSeducationCiencias Exactas y NaturalesSOUTHWESTERN GONDWANA0105 earth and related environmental sciencesEarth-Surface Processesgeographyeducation.field_of_studygeography.geographical_feature_categoryVolcanic arcGeologySOUTHERN PATAGONIAN ANDESGondwanaANTARCTIC PENINSULANUNATAK VIEDMANunatak ViedmaCIENCIAS NATURALES Y EXACTASGeology
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Hydrothermalism in the Tyrrhenian Sea: Inorganic and microbial sulfur cycling as revealed by geochemical and multiple sulfur isotope data

2011

15 pages; International audience; The Palinuro volcanic complex and the Panarea hydrothermal field, both located in the Tyrrhenian Sea (Italy), are associated with island arc magmatism and characterized by polymetallic sulfide mineralization. Dissolved sulfide concentrations, pH, and Eh measured in porewaters at both sites reveal a variable hydrothermal influence on porewater chemistry. Multiple sulfur isotopic measurements for disseminated sulfides (CRS: chromium reducible sulfur) extracted from sediments at Palinuro yielded a broad range in δ34S range between −29.8 and +10.2‰ and Δ33S values between+0.015 and+0.134‰. In contrast, sediments at Panarea exhibit a much smaller range in δ34SCR…

010506 paleontologySulfide[SDE.MCG]Environmental Sciences/Global ChangesGeochemistrychemistry.chemical_elementDisproportionationengineering.material010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationchemistry.chemical_compoundδ34S[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMassive sulfide complexGeochemistry and PetrologyHydrothermalism14. Life underwaterMultiple sulfur isotopesSulfate0105 earth and related environmental scienceschemistry.chemical_classificationgeographygeography.geographical_feature_categorySulfur cyclingGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySulfur[ SDE.MCG ] Environmental Sciences/Global ChangeschemistryVolcano13. Climate actionengineeringPyriteGeologyChemical Geology
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After the emergence of the Acheulean at Melka Kunture (Upper Awash, Ethiopia): From Gombore IB (1.6 Ma) to Gombore Iγ (1.4 Ma), Gombore Iδ (1.3 Ma) a…

2021

International audience; While the emergence of the Acheulean is well documented in East Africa at ~1.7 Ma, subsequent developments are less well understood and to some extent controversial. Here, we provide robust evidence regarding the time period between 1.6 Ma and 1.2 Ma, based on an interdisciplinary approach to the stratigraphic sequences exposed in the Gombore gully of Melka Kunture, in the upper Awash Valley of Ethiopia. Throughout the Pleistocene, the environment differed significantly from elsewhere in Africa because of the elevation at 2000 m asl, the cooler and rainy climate, the Afromontane vegetation, the development of endemic animal species, and the recurrent impact of volcan…

010506 paleontologybiologyPleistoceneMelka KuntureVegetationHomo erectus/Ergaster adaptation010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesArchaeologyGeographyVolcanismHuman evolution[SHS.ENVIR]Humanities and Social Sciences/Environmental studiesEast africaPeriod (geology)Assemblage (archaeology)Homo erectusLower PleistoceneComputingMilieux_MISCELLANEOUSAcheuleanAcheulean0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary International
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