Search results for "volcanism"

showing 10 items of 90 documents

Mercury concentration, speciation and budget in volcanic aquifers: Italy and Guadeloupe (Lesser Antilles)

2009

Abstract Quantifying the contribution of volcanism to global mercury (Hg) emissions is important to understand the pathways and the mechanisms of Hg cycling through the Earth's geochemical reservoirs and to assess its environmental impacts. While previous studies have suggested that degassing volcanoes might contribute importantly to the atmospheric budget of mercury, little is known about the amount and behaviour of Hg in volcanic aquifers. Here we report on detailed investigations of both the content and the speciation of mercury in aquifers of active volcanoes in Italy and Guadeloupe Island (Lesser Antilles). In the studied groundwaters, total Hg (THg) concentrations range from 10 to 500…

Basaltgeographygeography.geographical_feature_categorychemistry.chemical_elementMineralogyAquiferVolcanismHydrothermal circulationMercury (element)GeophysicsVolcanochemistryGeochemistry and PetrologyTRACEREnvironmental chemistryspeciation volcanic aquifers total and dissolved mercury mercury cycling volatile budgetWater qualityGeologyJournal of Volcanology and Geothermal Research
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Chemo-probe into the mantle origin of the NW Anatolia Eocene to Miocene volcanic rocks: Implications for the role of, crustal accretion, subduction, …

2017

Post-collisional Cenozoic magmatic activity in NW Anatolia produced widespread volcanism across the region. In the Biga Peninsula, in the west, medium-K calc-alkaline to ultra-K rocks with orogenic geochemical signature were emplaced at similar to 43-15 Ma (Biga orogenic volcanic rocks; BOVR). Volcanic activity in the Central Sakarya region, to the east, is mainly restricted to-53-38 Ma, but also continued during the Early Miocene with small basaltic extrusives (Sakarya orogenic volcanic rocks; SOVR). This study presents a new set of geochemical data (whole rock major and trace elements and Sr-Nd-Pb isotopic compositions), obtained from the Cenozoic calc-alkaline volcanic rocks from these t…

Basaltgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesbiologySubductionGeochemistryGeologyVolcanism010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesMantle (geology)Volcanic rockVolcano13. Climate actionGeochemistry and PetrologyMagmatismLileGeology0105 earth and related environmental sciencesLithos
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Fluid escape structures in the Graham Bank region (Sicily Channel, Central Mediterranean) revealing volcanic and neotectonic activity

2016

In the Sicily Channel, (Central Mediterranean), two geodynamic processes overlap each other, the Maghrebides- Apennines accretionary prism and the Sicily Channel rift. Moreover, the northwestern sector (Banks sector) is characterised by an irregular seafloor morphology linked to the recent volcanic and tectonic activity.In order to discriminate the role exerted by both the processes in the morphostructural setting of the area we used a dataset of both high and very high resolution single-channel and multi-channel profiles, acquired in the frame of the RITMARE project respectively with CHIRP and sparker, and airgun sources, and high resolution (5 m cell) morpho-bathymetric data. The data all…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaFluid escape volcanism neotectonics
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Waveforms clustering and single-station location of microearthquake multiplets recorded in the northern Sicilian offshore region

2013

In 2009 December, the OBSLab-INGV (Istituto Nazionale di Geofisica e Vulcanologia) deployed an Ocean Bottom Seismometer with Hydrophone (OBS/H) near the epicentral area of the main shock of the Palermo seismic sequence of 2002. The monitoring activity had a total duration of about 8 months. During this experiment, the OBS/H recorded 247 very local microearthquakes, whose local magnitude is between -0.5 and 2.5 and TS - TP delay time between 0.2 and 5 s, almost all ofwhichwere undetected by the Italian National Seismic Network. This local microseismicity has been analysed using an innovative clustering technique that exploits the similarity between the waveforms generated by different events…

Earthquake source observationSettore GEO/10 - Geofisica Della Terra SolidaSingle stationlanguage.human_languageComputational seismologySeismicity and tectonicGeophysicsGeochemistry and PetrologylanguageWaveformSubmarine tectonics and volcanismSubmarine pipelineSeismic monitoring and test-ban treaty verificationMicroearthquakeCluster analysisSicilianGeologySeismologyComputational seismologyGeophysical Journal International
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The evolution of a dynamic geological system: the support of a GIS for geochemical measurements at the fumarole field of Vulcano, Italy

1997

The island of Vulcano (Aeolian arc, Southern Italy) has displayed several periods of volcanic unrest since the end of the last eruption (1890). We report here results obtained from a long-term survey concerning variations of both the steam output and the exhaling surface area at the summit crater fumarolic field of La Fossa. The field measurements analysed in a Geographical Information System (GIS) show a highly dynamic volcanic system in which deep variations in the geochemistry and the temperature of the released fluids were accompanied by fluctuations in the mass output of steam and the topography of the crater field. The use of a GIS facilitated digitized reconstructions of maps of the …

geographygeography.geographical_feature_categoryVolcanic arcGeochemistryFluxVolcanismFumaroleGeophysicsVolcanoImpact craterGeochemistry and PetrologyMagmaAeolian processesGeologySeismologyJournal of Volcanology and Geothermal Research
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2017

Strombolian volcanism is a ubiquitous form of activity, driven by the ascent and bursting of bubbles of slug morphology. Whilst considerable attention has been devoted to understanding the behaviour of individual slugs in this regime, relatively little is known about how inter-slug interactions modify flow conditions. Recently, we reported on high temporal frequency strombolian activity on Etna, in which the larger erupted slug masses were followed by longer intervals before the following explosion than the smaller bursts (Pering et al., 2015). We hypothesised that this behaviour arose from the coalescence of ascending slugs causing a prolonged lag before arrival of the next distinct bubble…

Coalescence (physics)geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesbiologySlugBubbleVolcanismMechanics010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesStrombolian eruptionGeophysicsElectrical conduitVolcanoGeochemistry and PetrologyGas slugSeismologyGeology0105 earth and related environmental sciencesJournal of Volcanology and Geothermal Research
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Geochemical modeling of mixing between magmatic and hydrothermal gases: the case of Vulcano Island, Italy

1999

Abstract In this study we present a geochemical approach to model the mixing of magmatic and hydrothermal gases. Our model is based on a rigorous formulation of a perfectly dimensioned system of mass and energy balance equations. Inputs of the equation set are the H2O and CO2 content and gas emission temperature at the surface, together with some constraints gained from the chemical–physical features of the hydrothermal system. The output data give the composition of magmatic gas, mixing fractions and temperatures of gas mixtures in the mixing zone. The comparison of the emission temperature of fumarolic gases with their calculated mixing temperatures provides valuable indications on the ex…

geographyEquation of stategeography.geographical_feature_categoryMineralogyVolcanismHydrothermal circulationFumaroleGeophysicsVolcanoSpace and Planetary ScienceGeochemistry and PetrologyMagmaEarth and Planetary Sciences (miscellaneous)GeologyMixing (physics)Geochemical modelingEarth and Planetary Science Letters
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Volcanic Lakes in Africa: The VOLADA_Africa 2.0 Database, and Implications for Volcanic Hazard

2021

Volcanic lakes pose specific hazards inherent to the presence of water: phreatic and phreatomagmatic eruptions, lahars, limnic gas bursts and dispersion of brines in the hydrological network. Here we introduce the updated, interactive and open-access database for African volcanic lakes, country by country. The previous database VOLADA (VOlcanic LAke DAta Base, Rouwet et al., Journal of Volcanology and Geothermal Research, 2014, 272, 78–97) reported 96 volcanic lakes for Africa. This number is now revised and established at 220, converting VOLADA_Africa 2.0 in the most comprehensive resource for African volcanic lakes: 81 in Uganda, 37 in Kenya, 33 in Cameroon, 28 in Madagascar, 19 in Ethiop…

geographyVolcanic hazardsgeography.geographical_feature_categoryRiftDatabaseLake NyosScienceLimnologyQVolcanismmaarcomputer.software_genreMaarhazard assessmentVolcanoAfricaAfrica volcanic lakes maar Lake Nyos database hazard assessmentPhreatomagmatic eruptionGeneral Earth and Planetary SciencesScoriacomputervolcanic lakesdatabaseFrontiers in Earth Science
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Constraints on mantle source and interactions from He-Sr isotope variation in Italian Plio-Quaternary volcanism.

2008

[1] Helium isotope ratios of olivine and pyroxene phenocrysts from Plio-Quaternary volcanic rocks from southern Italy (seven Aeolian Islands, Mt. Vulture, Etna, Ustica, and Pantelleria) range from 2.3 to 7.1 Ra. Importantly, the phenocryst 3He/4He correlate well with whole rock Sr isotopic composition (0.70309– 0.70711), reflecting the mixing of two sources. A significant contribution of He from crustal contamination is recorded only occasionally (e.g., pyroxenes from Vulcano). When merged with data from the Roman Comagmatic Province, a remarkably strong near-linear He-Sr isotope correlation is apparent. The general northward decrease in 3He/4He corresponds to an increase in 87Sr/86Sr (and …

fluid inclusionheliumstrontiumitalian volcanism.Settore GEO/08 - Geochimica E Vulcanologia
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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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