Search results for " geochemistry"

showing 10 items of 1580 documents

Italica (Seville, Spain): use of local marble in Augustan age

2010

This study concerns 51 marble finds made of “Cipollino verde” coming from the ancient city of Italica (north of the modern city of Santiponce, 9 km NW of Seville, Spain), the earliest Roman settlement in Spain, founded in 206 B.C. The aim of this work was to determine their provenance from Greek and Italian quarries or from local quarries worked in the Iberian Peninsula. Thin-section optical microscopy, X-ray powder diffraction, bulk rock chemistry and O, C and Sr stable isotope analyses were carried out. Results were compared with literature data on “Cipollino verde” marbles quarried in southern Euboea (Greece), Apuan Alps (Italy), Almería, Extremoz, Seville (Spain) and Évora (Portugal). T…

“Cipollino verde” marble; mineralogy; petrography; geochemistry; stable isotopes; Italica; Spainarchaeometry; cipollino verde marble; mineralogy; stable isotopes; spain; italica; roman age; clay samples; pottery; viminacium; petrography; cipollino verde" marble; geochemistrySpainstable isotope“Cipollino verde” marblemineralogyItalicaSettore GEO/09 -Georis. Miner.e Appl.Mineral.-Petrogr. per l'Ambi.ed i B.Cult.petrographygeochemistry
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Coupled petrological-geodynamical modeling of a compositionally heterogeneous mantle plume

2018

Abstract Self-consistent geodynamic modeling that includes melting is challenging as the chemistry of the source rocks continuously changes as a result of melt extraction. Here, we describe a new method to study the interaction between physical and chemical processes in an uprising heterogeneous mantle plume by combining a geodynamic code with a thermodynamic modeling approach for magma generation and evolution. We pre-computed hundreds of phase diagrams, each of them for a different chemical system. After melt is extracted, the phase diagram with the closest bulk rock chemistry to the depleted source rock is updated locally. The petrological evolution of rocks is tracked via evolving chemi…

Chemical processgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciences010502 geochemistry & geophysics01 natural sciencesMantle (geology)Mantle plumePlumeGeophysicsVolcanoSource rockPetrologyGeothermal gradientGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPhase diagramTectonophysics
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Permian-Triassic Osteichthyes (bony fishes): diversity dynamics and body size evolution

2014

The Permian and Triassic were key time intervals in the history of life on Earth. Both periods are marked by a series of biotic crises including the most catastrophic of such events, the end-Permian mass extinction, which eventually led to a major turnover from typical Palaeozoic faunas and floras to those that are emblematic for the Mesozoic and Cenozoic. Here we review patterns in Permian-Triassic bony fishes, a group whose evolutionary dynamics are understudied. Based on data from primary literature, we analyse changes in their taxonomic diversity and body size (as a proxy for trophic position) and explore their response to Permian-Triassic events. Diversity and body size are investigate…

Extinction event010506 paleontologybiologyPermianPaleozoicEcologyNeopterygiiEarly TriassicActinopterygii010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesGeneral Biochemistry Genetics and Molecular BiologyPaleontologyHolosteiMesozoicGeneral Agricultural and Biological Sciences0105 earth and related environmental sciencesBiological Reviews
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Characterisation of the magmatic signature in gas emissions from Turrialba Volcano, Costa Rica

2014

The equilibrium composition of volcanic gases with their magma is often overprinted by interaction with a shallow hydrothermal system. Identifying the magmatic signature of volcanic gases is critical to relate their composition to properties of the magma (temperature, fO2, gas-melt segregation depth). We report measurements of the chemical composition and flux of the major gas species emitted from Turrialba Volcano during March 2013. Measurements were made of two vents in the summit region, one of which opened in 2010 and the other in 2012. We determined an average SO2 flux of 5.2 ± 1.9 kg s-1 using scanning ultraviolet spectroscopy, and molar proportions of H2O, CO2, SO2, HCl, CO and H2 ga…

010504 meteorology & atmospheric sciencesStratigraphyChemical compositionContinuous emissionSoil ScienceMineralogyVolcanoe010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationVolcanic GasesHydrothermal systemFlux (metallurgy)lcsh:StratigraphyMagmatic signaturesGeochemistry and PetrologyUltraviolet spectroscopyeventGas compositionFourier transform infrared spectroscopyChemical compositionlcsh:QE640-6990105 earth and related environmental sciencesEarth-Surface Processesevent.disaster_typegeographygeography.geographical_feature_categorylcsh:QE1-996.5Fourier transform infrared spectrometryPaleontologyFourier transform infrared spectroscopyGeologyChemical signatureGas-sensing systemlcsh:GeologyGeophysicsVolcanoCarbon dioxideSulfur dioxide13. Climate actionEquilibrium compositionMagmaCarbon dioxide; Fourier transform infrared spectroscopy; Sulfur dioxide; Ultraviolet spectroscopy; Volcanoes; Chemical compositions; Chemical signatures; Continuous emission; Equilibrium compositions; Fourier transform infrared spectrometry; Gas-sensing systems; Hydrothermal system; Magmatic signaturesGeology
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Active Degassing of Deeply Sourced Fluids in Central Europe: New Evidences From a Geochemical Study in Serbia

2021

We report on the results of an extensive geochemical survey of fluids released in the Vardar zone (central-western Serbia), a mega-suture zone at the boundary between Eurasia and Africa plates. Thirty-one bubbling gas samples are investigated for their chemical and isotopic compositions (He, C, Ar) and cluster into three distinct groups (CO2-dominated, N2-dominated, and CH4-dominated) based on the dominant gas species. The measured He isotope ratios range from 0.08 to 1.19 Ra (where Ra is the atmospheric ratio), and reveal for the first time the presence of a minor (<20%) but detectable regional mantle-derived component in Serbia. δ13C values range from −20.2‰ to −0.1‰ (versus PDB), with…

010504 meteorology & atmospheric sciencesGeochemistrycarbon dioxidecarbon central Europe deep fluids fractionation helium mantlehelium010502 geochemistry & geophysics01 natural sciencesMantle (geology)chemistry.chemical_compoundGeophysicschemistrydeep fluidsGeochemistry and PetrologyCarbon dioxidecentral EuropefractionationGeologymantle0105 earth and related environmental sciences
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Foreword for the thematic volume of the 8ISCPP. Recent advances in present and past cephalopod studies.

2012

3 pages, éditorial.; International audience

[ SDV.BID ] Life Sciences [q-bio]/Biodiversity010506 paleontology[ SDE.BE ] Environmental Sciences/Biodiversity and EcologybiologyPaleontology[SDV.BID]Life Sciences [q-bio]/Biodiversity010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCephalopod[SDE.BE] Environmental Sciences/Biodiversity and EcologyOceanographyThematic mapGeographySpace and Planetary Science[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology[SDE.BE]Environmental Sciences/Biodiversity and Ecology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesVolume (compression)[SDV.BID] Life Sciences [q-bio]/Biodiversity[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology
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Hydrothermal circulation on Ischia Island (Southern Italy), revealed by an integrated geochemical, geophysical and geological approach

2011

Volcano-hosted hydrothermal systems are complex geological objects, whose thorough characterisation requires extensive and interdisciplinary work. Indeed, even thought geological, geochemical and geophysical observations offer highly significant but independent information, only an integrated multidisciplinary approach can yield a comprehensive characterisation of the chemical/physical structure of hydrothermal systems. Notwithstanding the extensive application of geological, geochemical and geophysical techniques in geothermal research, there are only a few examples in the literature of concurrent use of the three techniques [Finizola et al., 2002; Zlotnicki et al., 2009]; these studies ov…

fluid geochemistryhydrothermal systemresurgent caldera.TEMERTIschiaSettore GEO/08 - Geochimica E Vulcanologia
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Crystallization of late-stage MORB under varying water activities and redox conditions: Implications for the formation of highly evolved lavas and ox…

2018

Abstract In order to understand late magmatic processes that occur in the deep oceanic crust, we performed a phase-equilibria study in a representative late-stage system at a pressure of 200 MPa with a special focus on the role of water and oxygen fugacity. The starting composition for the experiments was evaluated based on a statistical approach using evolved fresh MORB glasses from the database PETDB highest in FeO and TiO2 (in average 17.92 wt% and 3.73 wt%, respectively), assumed to represent frozen liquids erupted at the seafloor generated by extensive differentiation of MORB. We conducted crystallization experiments in a range of temperatures from 850 to 1050 °C with water activities …

Olivine010504 meteorology & atmospheric sciencesGabbroGeochemistryGeologyLiquidusengineering.material010502 geochemistry & geophysics01 natural sciencesSeafloor spreadingGeochemistry and PetrologyMineral redox bufferOceanic crustengineeringPlagioclaseAmphiboleGeology0105 earth and related environmental sciencesLithos
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Experimental alteration of granitic rocks: Implications for the evolution of geothermal brines in the Upper Rhine Graben, Germany

2020

Abstract Geothermal energy exploitation in the Upper Rhine Graben (URG) chiefly has targeted faults and fractures within or connected with the crystalline basement, where hot fluids of c. 200 °C circulate at depths of c. 5 km. Formation fluids of the crystalline basement are highly saline, NaCl-dominated brines, whereas shallow crystalline basement water ( The trace element concentrations of the leachates are hereby related to the composition and stability of minerals in the rocks and can be directly linked to the proposed and observed dissolution processes at the different temperatures. In experiments with pure water at 70 °C, representing the recharge or infiltration conditions, water-roc…

AnalcimeRenewable Energy Sustainability and the EnvironmentChemistry0211 other engineering and technologiesGeochemistryGeology02 engineering and technologyengineering.material010502 geochemistry & geophysicsGeotechnical Engineering and Engineering GeologyFeldspar01 natural sciencesvisual_artIllitevisual_art.visual_art_mediumengineeringKaolinitePlagioclase021108 energyQuartzDissolutionBiotite0105 earth and related environmental sciencesGeothermics
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Challenging Darwin: Evolution of Triassic Conodonts and Their Struggle for Life in a Changing World

2017

Abstract The phylogeny and distribution of Triassic conodonts reveal many aspects of their natural history. Conodonts incorporate the morphologic response to temperature as well as to eustatic cycles. Speciation, radiation, and extinction are not fortuitous and evolution uses heterochrony (progenesis and neoteny) in response to stress-generating events. Proteromorphosis (reappearance of ancestral morphs) and paedomorphosis (retention of juvenile traits) is a reaction to sublethal environmental stress. This often follows radiation of fully developed forms in the recovery stage after extinction that timely matches transgressions. Evolutionary retrogradation (neoteny) during eustatic high stan…

Extinction010504 meteorology & atmospheric sciencesPermianbiologyLadinian010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesPaleontologyPluvialPeriod (geology)ConodontNeotenyGeologyPermian–Triassic extinction event0105 earth and related environmental sciences
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