0000000000180218

AUTHOR

S. Chiavetta

showing 2 related works from this author

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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The behaviour of zirconium, hafnium and rare earth elements during the crystallisation of halite and other salt minerals

2017

Abstract Halite crystals from Messinian and Tortonian evaporites from Sicily and Spain and current precipitated halite crystals and the relative parent brines (active evaporation systems) were investigated in order to evaluate the Zr, Hf and Rare Earth Element (REE) behaviour. Halite crystallisation from evaporating brines fractionates Zr, Hf and REE through a two-step process. During the first step, dissolved complexes of studied elements are scavenged onto the surfaces of crystallising halite. During the second step, elements are co-precipitated into the crystal lattice as it grows. The first step mechanism is determined by the dissolved REE speciation. In saltworks where carbonate-REE co…

010504 meteorology & atmospheric sciencesEvaporiteGeochemistryMineralogychemistry.chemical_elementengineering.material010502 geochemistry & geophysics01 natural sciencesGeochemistry and PetrologySettore CHIM/01 - Chimica AnaliticaZr/HfDissolution0105 earth and related environmental sciencesZirconiumRare-earth elementGeologyAuthigenicHaliteREESettore GEO/08 - Geochimica E VulcanologiaDiagenesisEvaporitechemistryengineeringHaliteSeawaterGeologyChemical Geology
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