Search results for "Petrografia"

showing 10 items of 92 documents

Trace elements and noble gases (He, Ne, Ar) isotopic study of Fuerteventura carbonatites: implications for their mantle source

FuerteventuraSettore GEO/07 - Petrologia E PetrografiaCanary Islandscarbonatitenoble gaseREESettore GEO/08 - Geochimica E Vulcanologia
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The composition of fluids stored in the central Mexican lithospheric mantle: Inferences from noble gases and CO2 in mantle xenoliths

2021

We present the first isotopic (noble gases and CO2) characterization of fluid inclusions coupled to Raman microspectroscopy analyses in mantle xenoliths from Central Mexico, a geodynamically complex area where the Basin and Range extension was superimposed on the Farallon subduction (terminated at 28 Ma). To characterize the isotopic signature of the Central Mexican lithospheric mantle, we focus on fluid inclusions entrapped in mantle xenoliths found in deposits of the Joya Honda maar (JH), a Quaternary monogenetic volcano belonging to the Ventura Espiritu Santo Volcanic Field (VESVF) in the state of San Luis Potosí (central Mexico). Thirteen ultramafic plagioclase-free xenoliths were selec…

GEO/07 - PETROLOGIA E PETROGRAFIA010504 meteorology & atmospheric sciencesCarbonate recyclingGeochemistry2010502 geochemistry & geophysics01 natural sciencesMantle (geology)chemistry.chemical_compoundNoble gaseGeochemistry and PetrologyUltramafic rockGEO/08 - GEOCHIMICA E VULCANOLOGIAXenolithFluid inclusionsMetasomatismFarallon Plate0105 earth and related environmental sciencesMantle refertilizationSubductionGeologyFluid inclusionSilicateCOchemistryCarbonate recycling CO2 Fluid inclusions Mantle refertilization Mexican mantle xenoliths Noble gasesGeologyMexican mantle xenolith
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Petrography and high-resolution geochemical records of Lower Jurassic manganese-rich deposits from Monte Mangart, Julian Alps

2016

Deposits with unusually high Mn contents sampled at Monte Mangart in the Julian Alps include organic-rich marlstone and black shale with interbedded manganoan and siliceous limestone, which were deposited during the early Toarcian Oceanic Anoxic Event. Mn enrichment during that period has been related to global sea-level change coincident with increasing subsidence rate. The formation of Fe-Mn nodules, marking a hardground at the base of the Monte Mangart section, seems to be triggered by release of Mn from remote hydrothermal vents into a region of relatively elevated submarine topography where oxidizing conditions prevailed. However, very high Mn contents in carbonate phases above the har…

GeochemistrySettore GEO/07 - Petrologia E PetrografiaPaleontologyengineering.materialOceanographyCarbonate hardgroundsEarly Toarcian Mn-bearing deposits Anoxic Event Stable isotope stratigraphy Rare earth elementsAnoxic watersDiagenesisSettore GEO/08 - Geochimica E VulcanologiaPetrographyEarth scienceschemistry.chemical_compoundPaleontologychemistryMarlengineeringCarbonatePyriteEarly Toarcian Mn-bearing deposits Anoxic Event Stable isotope stratigraphy Rare earth elementsEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesHydrothermal vent
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A radiometric and petrographic interpretation of discrepancies on uranium content in samples collected at Alte Madonie Mounts region (Sicily, Italy)

2013

Abstract The main goal of this work is to evaluate a correlation between anomalous Uranium (U) content and petrographic features of some soil and rock samples collected at Alte Madonie Mounts region (North-central Sicily, Italy). A total of 41 samples of selected soils and rocks were collected, powdered, dried and sealed in “Marinelli” beakers for 20 days before the measurement to ensure that radioactive equilibrium between 226 Ra and 214 Bi was reached. Gamma-ray spectrometric analysis was used to quantify radioactivity concentrations. Mineralogical and chemical features of the samples were determined by X-ray Fluorescence (XRF), X-ray Diffractometry (XRD), Attenuated Total Reflection-Four…

Geological PhenomenaSettore ING-IND/20 - Misure E Strumentazione NucleariHealth Toxicology and MutagenesisAnalytical chemistryMineralogyX-ray fluorescencechemistry.chemical_elementPetrographyRadiation MonitoringSoil Pollutants RadioactiveEnvironmental ChemistryRadiometryWaste Management and DisposalGamma ray spectrometryRadioisotopesSettore GEO/07 - Petrologia E PetrografiaGeneral MedicineUraniumPollutionSpectrometry GammaItalychemistryEnvironmental radioactivity Radiation monitoring Gamma-ray spectrometry X-rayfluorescence X-ray diffractometryEnergy dispersive spectrometrySoil waterUraniumEnvironmental radioactivityEnvironmental scienceRadiometric datingBismuthJournal of Environmental Radioactivity
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Temporal evolution of the Fogo Volcano magma storage system (Cape Verde Archipelago): a fluid inclusions perspective

2023

The architecture of the magma storage system underneath Fogo Volcano (Cape Verde Archipelago) is characterised using novel fluid inclusion results from fifteen basanites, spanning the last 120 thousand years of volcanic activity, and encompassing a major flank collapse event at -73 ka. Fluid inclusions, hosted in olivine and clinopyroxene, are made of pure CO2, and based on their textural characteristics, are distinguished in early (Type I) and late (Type II) stage. Inclusions homogenize to a liquid phase in the 2.8 to 30.8 degrees C temperature range. Densities values, recalculated assuming an original 10% H2O content at the time of trapping, range from 543 to 952 kg center dot m(-3), and …

GeophysicsMagmatic systemGeochemistry and PetrologySettore GEO/07 - Petrologia E PetrografiaOceanic island volcanismBasanitesMagma ascent pathSettore GEO/08 - Geochimica E VulcanologiaJournal of Volcanology and Geothermal Research
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La Grotta dei Personaggi di Montevago (AG), una nuova segnalazione di cavità ipogenica in Sicilia

2015

La Grotta dei Personaggi è localizzata in Sicilia occidentale, nei pressi di Monte Magaggiaro, a S del centro abitato di Montevago (AG). Nell’area sono presenti sorgenti termali, caratterizzate da acque cloro-solfate alcalino-terrose con temperatura di circa 40 °C e pH 7. La Grotta dei Personaggi, conosciuta già dai primi anni del 1900 e nota anche per ritrovamenti archeologici, non era mai stata dettagliatamente rilevata e studiata. La cavità si sviluppa prevalentemente in calcari di piattaforma della formazione Inici (Giurassico inf.) e in calcari di scarpata e pelagici della formazione Buccheri (Giurassico inf.-sup.). Si tratta di una cavità sub-orizzontale che presenta uno sviluppo di c…

Grotta ipogenica Grotta dei Personaggi Monte Magaggiaro SiciliaSettore GEO/04 - Geografia Fisica E GeomorfologiaSettore GEO/07 - Petrologia E PetrografiaSettore BIO/05 - Zoologia
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Fumarolic alteration products of three hydrothermal areas of Greece: Chemical characterization and environmental impact.

2018

Samples of efflorescences and encrustations of hydrothermal origin have been collected at three fumarolic areas in Greece. The three sites are Sousaki, Thiafi (Methana) and Kokkino Nero (Kos) and all belong to the South Aegean Active Volcanic Arc. Samples were analysed for their mineralogical (XRD and SEM-EDS) and chemical composition. Solutions obtained from both mineralization with HNO3 and leaching with distilled water, were analysed for major (ICP-OES), minor and trace metals (ICP-MS) and for sulfate contents (IC). Results show that their composition is mainly controlled by the petrological composition of the substrate (ultramafic rocks at Sousaki, felsic volcanic rocks at Methana and l…

Hydrothermal alteration products sulfates toxic metals.Settore GEO/07 - Petrologia E PetrografiaSettore GEO/08 - Geochimica E Vulcanologia
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Volatiles in pantellerite magmas: A case study of the Green Tuff Plinian eruption (Island of Pantelleria, Italy)

2013

Abstract The Green Tuff (GT) Plinian eruption, the largest in magnitude at Pantelleria, erupted 3 to 7 km3 DRE of pantellerite magma and a small volume of trachyte. Fifty-nine anorthoclase-hosted melt inclusions from the two basal pumice members were analyzed by FT-IR spectroscopy in order to assess the pre-eruptive H2O content in the pantellerite melt. Microanalytical methods were used to determine major element, Cl, F and S contents. Melt inclusions and glassy groundmasses have a nearly homogeneous pantelleritic composition (peralkaline index = 1.9-2.2) and variable water contents ranging from 1.4 to as high as 4.2 wt %, i.e. much higher than the 1.4 wt % of earlier published studies. The…

LavaSettore GEO/07 - Petrologia E PetrografiaGeochemistryTrachyteMagma chamberStrombolian eruptionGeophysicsEffusive eruptionGeochemistry and PetrologyPumiceMagmaThe Green Tuff (GT) Plinian eruption the largest in magnitude at Pantelleria erupted 3 to 7 km 3 DRE of pantellerite magma and a small volume of trachyte. Fifty-nine anorthoclase-hosted melt inclusions from the two basal pumice members were analyzed by FT-IR spectroscopy in order to assess the pre-eruptive H2Ocontent in the pantellerite melt. Microanalytical methods were used to determine major element Cl F and S contents. Melt inclusions and glassy groundmasses have a nearly homogeneous pantelleritic composition (peralkaline index = 1.9-2.2) and variable water contents ranging from 1.4 to as high as 4.2 wt % i.e. much higher than the 1.4 wt % of earlier published studies. The chlorine content is constant at about 1 wt %. Combined Cl and H2O data were used to estimate a confining pressure of about 50 MPa (depth around 2-3 km) for the GT magma chamber. The chamber was characterized by a compositional zoning with a dominant pantellerite overlying a trachyte magma. Soon after the GT eruption intra-caldera volcanism was dominated by the eruption of voluminous trachyte lavaflows while pantellerite melt production resumed after about 20 ka with numerous low-volume mildly explosive (Strombolian) to effusive eruptions. Comparison with data from the literature reveals that despite the differentexplosivity the post-caldera Strombolian eruptions and the GT Plinian eruption were fed by pantelleritic magmas with similar water contents. Chlorine and CO2contents suggest that the young magma reservoirs feeding the Strombolian to effusive activity were deeper (h≥4.5 km) than the much larger (based on erupted volumes) magma chamber which fed the GT eruptionGeologyMelt inclusionsJournal of Volcanology and Geothermal Research
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Evolution of the magma system of Pantelleria (Italy) from 190 ka to present

2022

The eruptive history of Pantelleria has been marked by the eruption of nine peralkaline ignimbrites, with inter-ignimbrite episodes from small, local volcanic centres. New whole-rock geochemical data are presented for seven ignimbrites and used with published data for younger units to track compositional changes with time. From»190 ka, silicicmagmatismwas dominated by comenditic trachyte to comendite compositions, evolving along generally similar liquid lines of descent (LLOD). The final ignimbrite, the Green Tuff (»46 ka), was tapped from a compositionally zoned pantelleritic upper reservoir to a trachytic mush zone. Younger (20–7 ka) silicic magmatism has been relatively small scale, with…

MagmaSettore GEO/07 - Petrologia E PetrografiaPantelleria Ignimbrite Magma reservoirs Compositional changes with time Comendite Pantellerite.General Earth and Planetary SciencesPetrologyGeologyGeneral Environmental ScienceComptes Rendus. Géoscience
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Water solubility in trachytic and pantelleritic melts: an experimental study

2021

International audience; Solubility experiments were performed on a trachyte and a pantellerite from Pantelleria. The trachyte has SiO 2 = 65.2 wt%, Al 2 O 3 = 15.2 wt% and a peralkaline index (P.I. = molar[(Na 2 O + K 2 O)/Al 2 O 3 ]) ∼ 1 while the pantellerite has SiO 2 = 72.2 wt%, Al 2 O 3 = 11 wt% and a P.I. = 1.3. Solubility experiments were performed in the pressure range of 50-300 MPa at T = 950°C for the trachyte and 50-200 MPa at T = 850°C for the pantellerite. The water content of experimental glasses was determined by Karl Fischer titration, elemental analyser and FT-IR spectroscopy. Water content appears similar in both compositions for analogous pressure conditions, varying from…

Materials scienceAqueous solutionWater solubility010401 analytical chemistrySettore GEO/07 - Petrologia E Petrografia[SDU.STU]Sciences of the Universe [physics]/Earth SciencesTrachyte010502 geochemistry & geophysics01 natural sciencesTrachyte0104 chemical sciencesChemical engineering[SDU]Sciences of the Universe [physics]General Earth and Planetary SciencesExperimentsAlkaline magmasPantelleriteTrachyte PantelleriteWater solubility Experiments Alkaline magmas0105 earth and related environmental sciencesGeneral Environmental ScienceComptes Rendus. Géoscience
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