Search results for "Medium"

showing 10 items of 3746 documents

Phase Relations, Reaction Sequences and Petrochronology

2017

At the core of petrochronology is the relationship between geochronology and the petrological evolution of major mineral assemblages. The focus of this chapter is on outlining some of the available strategies to link inferred reaction sequences and microstructures in metamorphic rocks to the ages obtained from geochronology of accessory minerals and datable major minerals. Reaction sequences and mineral assemblages in metamorphic rocks are primarily a function of pressure ( P ), temperature ( T ) and bulk composition ( X ). Several of the major rock-forming minerals are particularly sensitive to changes in P–T (e.g., garnet, staurolite, biotite, plagioclase), but their direct geochronology …

010504 meteorology & atmospheric sciencesMetamorphic rockGeochemistrySubduction zone metamorphismMetamorphic reaction010502 geochemistry & geophysics01 natural sciencesGeochemistry and Petrologyvisual_artStauroliteGeochronologyvisual_art.visual_art_mediumIsogradProtolithGeology0105 earth and related environmental sciencesZirconReviews in Mineralogy and Geochemistry
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Quantifying geological uncertainty in metamorphic phase equilibria modelling; a Monte Carlo assessment and implications for tectonic interpretations

2016

AbstractPseudosection modelling is rapidly becoming an essential part of a petrologist's toolkit and often forms the basis of interpreting the tectonothermal evolution of a rock sample, outcrop, or geological region. Of the several factors that can affect the accuracy and precision of such calculated phase diagrams, “geological” uncertainty related to natural petrographic variation at the hand sample- and/or thin section-scale is rarely considered. Such uncertainty influences the sample's bulk composition, which is the primary control on its equilibrium phase relationships and thus the interpreted pressure–temperature (P–T) conditions of formation. Two case study examples—a garnet–cordierit…

010504 meteorology & atmospheric sciencesMetamorphic rockMonte Carlo methodMineralogyPseudosectionEarth and Planetary Sciences(all)3705 Geologysub-05010502 geochemistry & geophysics01 natural sciencesKyaniteGeological uncertaintyMatrix (geology)ErrorPetrographyMonte Carlo0105 earth and related environmental sciencesMnNCKFMASHTOlcsh:QE1-996.5Schist37 Earth Scienceslcsh:GeologyTectonicsvisual_artStaurolitevisual_art.visual_art_mediumGeneral Earth and Planetary Sciences3706 GeophysicsGeologyGeoscience Frontiers
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Cretaceous ultrapotassic magmatism from the Sava-Vardar Zone of the Balkans

2020

Highlights • Geochemically diverse Late Cretaceous small-volume magmatism in the Sava-Vardar Zone. • Late Cretaceous ultrapotassic lava, equivalent of minette and kersantite. • Magma derivation from a LREE and K enriched, garnet-bearing anciently metasomatized mantle source. • Magmatism occurred either in a fore-arc setting or is associated with transtensional tectonics. Abstract Late Cretaceous global plate reorganization associated with the inception of counterclockwise rotation of Africa relative to Europe initiated in the Balkan region small-volume magmatism of diverse geochemical signature along the enigmatic Sava-Vardar Zone. We study a Late Cretaceous lamprophyric sill in Ripanj vill…

010504 meteorology & atmospheric sciencesSava-Vardar zoneGeochemistryengineering.material010502 geochemistry & geophysicsFeldspar01 natural sciencesMantle (geology)Cretaceous ultrapotassic rocksSillGeochemistry and PetrologySava-Vardar zonaMesozoic0105 earth and related environmental sciencesMantle metasomatismgeographygeography.geographical_feature_categorySubductionKredne ultrakalijske steneGeologyDurbachite-vaugnerite serijaReconstruction geochemistryCretaceousDurbachite-vaugnerite series13. Climate actionvisual_artMagmatismengineeringvisual_art.visual_art_mediumPhlogopiteGeologymetasomatizam omotača
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Eco-Friendly Estimation of Heavy Metal Contents in Grapevine Foliage Using In-Field Hyperspectral Data and Multivariate Analysis

2019

Heavy metal monitoring in food-producing ecosystems can play an important role in human health safety. Since they are able to interfere with plants’ physiochemical characteristics, which influence the optical properties of leaves, they can be measured by in-field spectroscopy. In this study, the predictive power of spectroscopic data is examined. Five treatments of heavy metal stress (Cu, Zn, Pb, Cr, and Cd) were applied to grapevine seedlings and hyperspectral data (350−2500 nm), and heavy metal contents were collected based on in-field and laboratory experiments. The partial least squares (PLS) method was used as a feature selection technique, and multiple linear regressions (…

010504 meteorology & atmospheric sciencesScience010501 environmental sciences01 natural sciencesMetalHuman healthLinear regressionPartial least squares regressionSpectroscopyheavy metals0105 earth and related environmental sciencesChemistrysvmQfungifield spectroscopy; hyperspectral; heavy metals; grapevine; PLS; SVM; MLRHyperspectral imagingfood and beveragesHeavy metalsplsEnvironmentally friendlyfield spectroscopygrapevinemlrhyperspectralvisual_artEnvironmental chemistryvisual_art.visual_art_mediumGeneral Earth and Planetary SciencesRemote Sensing; Volume 11; Issue 23; Pages: 2731
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Integrated biomonitoring of airborne pollutants over space and time using tree rings, bark, leaves and epiphytic lichens

2016

The integrated use of tree rings and outer tissues, and lichens, was tested for monitoring how pollutant concentrations vary in space and over time nearby an incinerator in industrial area in Central Italy. Trace elements in thalli of lichen Xanthoria parietina and in leaves, bark, wood of Quercus pubescens, as well as carbon, oxygen and nitrogen isotope ratios in tree rings were analyzed. Some trace elements in the leaves differed significantly between the plots, though this was not the case in lichens and bark. The values of δ13C and δ18O showed the same trend in all plots, while the values of δ15N were higher in the distal plot. The results indicated that trace elements were intercepted …

010504 meteorology & atmospheric sciencesSoil Science010501 environmental sciencesQuercus pubescens01 natural sciencesXanthoria parietinaBiomonitoringBotanyDendrochronologyFoliose thalliLichen0105 earth and related environmental sciencesEcologybiologyTree ringsXylemForestrybiology.organism_classificationPollutionStable isotopeThallusvisual_artBiomonitoringvisual_art.visual_art_mediumBarkDendrochemistry
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2019

Abstract. The flow of fluids through porous media such as groundwater flow or magma migration is a key process in geological sciences. Flow is controlled by the permeability of the rock; thus, an accurate determination and prediction of its value is of crucial importance. For this reason, permeability has been measured across different scales. As laboratory measurements exhibit a range of limitations, the numerical prediction of permeability at conditions where laboratory experiments struggle has become an important method to complement laboratory approaches. At high resolutions, this prediction becomes computationally very expensive, which makes it crucial to develop methods that maximize …

010504 meteorology & atmospheric sciencesStratigraphyFinite differencePaleontologySoil ScienceReynolds numberGeologyMechanics010502 geochemistry & geophysics01 natural sciencesStencilNon-Newtonian fluidPhysics::GeophysicsPhysics::Fluid DynamicsPermeability (earth sciences)symbols.namesakeGeophysicsGeochemistry and PetrologyFluid dynamicsNewtonian fluidsymbolsPorous mediumGeology0105 earth and related environmental sciencesEarth-Surface ProcessesSolid Earth
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Textural-chemical changes and deformation conditions registered by phyllosilicates in a fault zone (Pic de Port Vieux thrust, Pyrenees)

2017

International audience; Synkinematic phyllosilicates in fault zones can be used to deduce the deformation mechanisms and the conditions of fault activity, as their chemical composition, crystal structure and texture can record the different stages of deformation and fluid-rock interactions. The Pic de Port Vieux, a second-order thrust related to the major Gavarnie thrust in the southern central part of the Pyrenees Axial Zone, juxtaposes Triassic pelites of the hanging wall and Cretaceous limestones of the footwall. In order to investigate the mineralogical and geochemical changes and constrain the deformation conditions of thrusting, characterization of phyllosilicates was performed along …

010504 meteorology & atmospheric sciences[SDV]Life Sciences [q-bio]GeochemistryFault (geology)engineering.material010502 geochemistry & geophysics01 natural sciences[ SDE ] Environmental Scienceschemistry.chemical_compoundGeochemistry and PetrologyPeliteThrust faultQuartzChlorite0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryK-white micaThrust fault[ SDV ] Life Sciences [q-bio]MuscovitePyreneesGeologyHematitePhyllosilicatesFluid-rock interactionsDiagenesischemistry[SDU]Sciences of the Universe [physics]visual_art[SDE]Environmental Sciencesvisual_art.visual_art_mediumengineeringChloriteGeology[ SDU ] Sciences of the Universe [physics]
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Decrespignyite-(Y), a new copper yttrium rare earth carbonate chloride hydrate from Paratoo, South Australia

2002

AbstractDecrespignyite-(Y) is a new copper yttrium rare earth carbonate chloride hydrate from the Paratoo copper mine, near Yunta, Olary district, South Australia. Decrespignyite-(Y) occurs as blue crusts, coatings and fillings in thin fissures on the slatey country rock. Individual pseudohexagonal platelets are typically 10–50 µm in maximum dimension and are often curved. Associated minerals include caysichite-(Y), donnayite-(Y), malachite and kamphaugite-(Y). Electron microprobe and CHN analyses gave: Y2O3 42.2; La2O3 0.1; Pr2O3 0.1; Nd2O3 1.3; Sm2O3 1.0; Gd2O3 4; Tb2O3 0.4; Dy2O3 3.7; Ho2O3 2.6; Er2O3 2.5; CaO 0.5; CuO 10.9; Cl 3.0; CO2 19.8; H2O 10.8, yielding an empirical formula of (Y…

010504 meteorology & atmospheric scienceschemistry.chemical_elementMalachiteElectron microprobeYttrium010502 geochemistry & geophysics01 natural sciencesCopperchemistry.chemical_compoundCrystallographychemistryGeochemistry and Petrologyvisual_artvisual_art.visual_art_mediumPleochroismCarbonateHydratePowder diffraction0105 earth and related environmental sciencesMineralogical Magazine
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Phase equilibrium constraints on pre-eruptive conditions of recent felsic explosive volcanism at Pantelleria Island, Italy.

2010

International audience; We present experimental phase equilibria carried out on a pantelleritic bulk-rock composition with a peralkalinity index [PI = molar (Na2O + K2O)/Al2O3] = 1*4, which is representative of the most energetic pumice fall eruption of the resurgent post-caldera volcanism on Pantelleria island. For the explored conditions (P = 25-150 MPa; T = 680-800°C; H2Omelt up to 6 wt %; fO2 ≤ NNO, where NNO is nickel-nickel oxide buffer) clinopyroxene is the liquidus phase followed by alkali feldspar and then quartz. The crystallization of amphibole is limited to temperatures below 700°C. Aenigmatite crystallizes near the liquidus for P ≥ 100 MPa. When clinopyroxene is the sole liquid…

010504 meteorology & atmospheric sciencespantellerite[SDE.MCG]Environmental Sciences/Global Changeshydrous reduced magmaLiquidusengineering.material010502 geochemistry & geophysicsFeldspar01 natural sciencesPeralkaline rockAenigmatiteGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanologyphase equilibriaPetrologyGeomorphology0105 earth and related environmental sciencesMelt inclusionsFelsicSettore GEO/07 - Petrologia E PetrografiaGeophysics13. Climate actionvisual_artMagmaengineeringvisual_art.visual_art_mediumperalkaline magmatismAlkali feldsparGeologyPantelleria
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Impact of Coseismic Frictional Melting on Particle Size, Shape Distribution and Chemistry of Experimentally-Generated Pseudotachylite

2020

In natural friction melts, or pseudotachylites, clast textures and glass compositions can influence the frictional behavior of faults hosting pseudotachylites, and are, in turn, sensitive to the processes involved in pseudotachylite formation. Quantification of these parameters in situations where the host rock composition and formation conditions are well-constrained, such as analogue experiments, may yield calibrations that can be employed in analysis of natural pseudotachylites. In this paper, we experimentally-generated pseudotachylites in granitoid rocks (tonalite and Westerly granite) at Pconf= 40 MPa and slip rates of ∼0.1 m s−1, comparable to the conditions under which natural pseud…

010504 meteorology & atmospheric sciencessize and shape distributionfrictional meltingMineralogySlip (materials science)engineering.materialchemistry010502 geochemistry & geophysicsFeldspar01 natural sciencesexperimental pseudotachylitePlagioclaselcsh:ScienceQuartzgranite0105 earth and related environmental sciencestonaliteDecrepitationClastic rockvisual_artengineeringvisual_art.visual_art_mediumGeneral Earth and Planetary Scienceslcsh:QComminutionBiotiteFrontiers in Earth Science
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