0000000000154679

AUTHOR

Dario Cellura

showing 6 related works from this author

Geochemical characterization of surface waters and groundwater resources in the Managua area (Nicaragua, Central America)

2008

This paper reports new geochemical data on dissolved major and minor constituents in surface waters and ground waters collected in the Managua region (Nicaragua), and provides a preliminary characterization of the hydrogeochemical processes governing the natural water evolution in this area. The peculiar geological features of the study site, an active tectonic region (Nicaragua Depression) characterized by active volcanism and thermalism, combined with significant anthropogenic pressure, contribute to a complex evolution of water chemistry, which results from the simultaneous action of several geochemical processes such as evaporation, rock leaching, mixing with saline brines of natural or…

PollutionHydrologygeographygeography.geographical_feature_categorygroundwater chemistrymedia_common.quotation_subjectGeochemistryLessivageAquiferPollutionSettore GEO/08 - Geochimica E VulcanologiaSalinityGeochemistry and PetrologyEnvironmental ChemistryLeaching (agriculture)Surface waterGeothermal gradientGroundwaterGeologymedia_commonApplied Geochemistry
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Diffuse soil CO2 degassing from Linosa island

2014

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Volcano monitoringLineamentGeochemistrysoil degassingfluid geochemistryCO2lcsh:QC851-999Instruments and techniques; Soil degassing; Volcano monitoring; GeophysicsSequential Gaussian simulationSoil co2 fluxFlux (metallurgy)Soil degassingGeomorphologygeographygeography.geographical_feature_categoryRiftlcsh:QC801-809Instruments and techniquesSettore GEO/08 - Geochimica E VulcanologiaTectonicslcsh:Geophysics. Cosmic physicsGeophysicsVolcanoLinosaSoil CO_2 fluxlcsh:Meteorology. ClimatologyGeologyChannel (geography)
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Petrology and geochemistry of submarine volcanism in the Sicily Channel Rift

2006

Submarine magmatism in the Sicily Channel Rift began in the early Pliocene and lasted until almost 200 yr ago. We present here petrological and geochemical data on volcanic rocks dredged from Graham and Nameless banks and Pantelleria seamounts in the Pelagian sector of the Sicily Channel Rift. Petrological evidence suggests that the ascent of magmas to the surface was relatively rapid, probably through channels superimposed over the major tectonic discontinuities of the Rift. Major and trace element data indicate an ocean island basalt affinity for Graham and Nameless bank alkaline lavas and a depleted tholeiitic signature for one Pantelleria seamount, which had a shallower mantle source. S…

BasaltgeographyRiftgeography.geographical_feature_categoryRadiogenic nuclideSiciy Channel PAntelelriaSeamountSettore GEO/07 - Petrologia E PetrografiaGeochemistryGeologyOcean island basaltsicily channel riftMantle (geology)sr‐nd‐pb isotopesVolcanic rockMagmatismsicily channel rift; sr‐nd‐pb isotopes; submarine volcanismPetrologysubmarine volcanismGeology
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Submarine volcanism in the Sicily Channel: the messagge from a deep mantle reservoir.

2004

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Integrated geochemical and geophysical surveys for a study of sea-water intrusion

2009

geochemical analysisSettore GEO/11 - Geofisica Applicatasea intrusionMASWTDEMERTSettore GEO/08 - Geochimica E Vulcanologia
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Helium isotope constraints on the mantle source of OIB-type Na-alkaline magmatism in Southern Mediterranea

2007

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