Search results for "TAM"

showing 10 items of 11664 documents

Interpretation of the nitrogen isotopic composition of Precambrian sedimentary rocks: Assumptions and perspectives

2016

International audience; Nitrogen isotope compositions in sedimentary rocks (d(15)N(sed)) are routinely used for reconstructing Cenozoic N-biogeochemical cycling and are also being increasingly applied to understanding the evolution of ancient environments. Here we review the existing knowledge and rationale behind the use of d(15)N(sed) as a proxy for the Precambrian N-biogeochemical cycle with the aims of (i) identifying the major uncertainties that affect analyses and interpretation of nitrogen isotopes in ancient sedimentary rocks, (ii) developing a framework for interpreting the Precambrian d(15)N(sed) record, (iii) testing this framework against a database of Precambrian d(15)N(sed) va…

010504 meteorology & atmospheric sciencesEarth scienceNitrogen isotopesMetamorphismGeologyNitrogen biogeochemical cycle010502 geochemistry & geophysicsEarly Earth01 natural sciencesIsotopes of nitrogenDiagenesisPaleontologyPrecambrianGeologic time scale13. Climate actionGeochemistry and Petrology[SDU]Sciences of the Universe [physics]Ocean oxygenationSedimentary rock14. Life underwaterPrecambrianCenozoicGeology[ SDU ] Sciences of the Universe [physics]0105 earth and related environmental sciences
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High-grade metamorphism and partial melting of basic and intermediate rocks

2016

Rocks of basic and intermediate bulk composition occur in orogenic terranes from all geological time periods and are thought to represent significant petrological components of the middle and lower continental crust. However, the former lack of appropriate thermodynamic models for silicate melt, amphibole and clinopyroxene that can be applied to such lithologies at high temperature has inhibited effective phase equilibrium modelling of their petrological evolution during amphibolite- and granulite facies metamorphism. In this work, we present phase diagrams calculated in the Na2O–CaO–K2O–FeO–MgO–Al2O3–SiO2–H2O–TiO2–O2 (NCKFMASHTO) compositional system for a range of natural basic and interm…

010504 meteorology & atmospheric sciencesGeochemistryPartial meltingMetamorphismGeologySolidusengineering.material010502 geochemistry & geophysicsGranulite01 natural sciencesLewisian complexDioriteGeochemistry and PetrologyengineeringPetrologyAmphiboleGeology0105 earth and related environmental sciencesHornblendeJournal of Metamorphic Geology
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Comment on “Evolution of high-pressure mafic granulites and pelitic gneisses from NE Madagascar: Tectonic implications”. Tectonophysics, 662, 219–242…

2017

Abstract Determining the possible tectonic regimes active during the Neoproterozoic is crucial for the knowledge of the evolution of the super-continent Gondwana. In Madagascar, that occupies a key position in Gondwana, there is an on-going debate regarding the location of possible suture zones and the implications in terms of paleo-geography. Recognizing high-pressure to ultra-high pressure conditions in mafic rocks is commonly viewed as a strong argument for paleo-subduction zones. Ishwar-Kumar et al. (2015) report unusual high pressure conditions (24 kbar) in Neoproterozoic to Cambrian rocks from North-Central Madagascar (Andriamena Complex). They propose a geodynamic model in which exhu…

010504 meteorology & atmospheric sciencesGeochemistry[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/Petrography010502 geochemistry & geophysicsGranulite01 natural sciencesGondwanaGeophysics13. Climate actionFacies14. Life underwaterSuture (geology)MaficMetamorphic faciesGeologyComputingMilieux_MISCELLANEOUS[ SDU.STU.PE ] Sciences of the Universe [physics]/Earth Sciences/Petrography0105 earth and related environmental sciencesEarth-Surface ProcessesTerraneGneiss
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2021

Abstract Contaminated soils are lands in Europe deemed less favourable for conventional agriculture. To overcome the problem of their poor fertility, bio-fertilization could be a promising approach. Soil inoculation with a choice of biological species (e.g. earthworm, mycorrhizal fungi, diazotroph bacteria) can be performed in order to improve soil properties and promote nutrients recycling. However, questions arise concerning the dynamics of the contaminants in an inoculated soil. The aim of this study was to highlight the soil-plant-earthworm interactions in the case of a slightly contaminated soil. For this purpose, a pot experiment in controlled conditions was carried out during 2 month…

010504 meteorology & atmospheric sciencesHealth Toxicology and MutagenesisBiomass010501 environmental sciencesToxicologycomplex mixtures01 natural sciencesNutrient0105 earth and related environmental sciences2. Zero hungerbiologyChemistryEarthwormTrace elementfood and beveragesGeneral Medicine15. Life on landbiology.organism_classificationPollutionSoil contamination6. Clean waterBioavailability13. Climate actionEnvironmental chemistryBioaccumulationSoil waterEnvironmental Pollution
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Anthropogenic lead distribution in soils under arable land and permanent grassland estimated by Pb isotopic compositions

2008

International audience; The role of land use on fate of metals in soils is poorly understood. In this work, we studied the incorporation of lead in two neighboring soils with comparable pedogenesis but under long-term different agricultural management. Distributions of anthropogenic Pb were assessed from concentrations and isotopic compositions determined on bulk horizon samples, systematical 5–10 cm increment samples, and on 24-h EDTA extracts. Minor amounts of anthropogenic lead were detected until 1-m depth under permanent grassland, linked to high earthworm activity. In arable land, exogenous Pb predominantly accumulated at depths <60 cm. Although the proximity between the two sites ens…

010504 meteorology & atmospheric sciencesHealth Toxicology and MutagenesisMETAL POLLUTIONLANTHANUM010501 environmental sciencesToxicology01 natural sciencesanalyse de solIsotopesSoil PollutantsLAND USEIsotope analysis2. Zero hungerbiologySolid Phase ExtractionprairiePb ISOTOPIC COMPOSITIONSAgricultureGeneral Medicineanalyse comparativePollutionSoil contaminationDeposition (aerosol physics)Environmental chemistryFranceArable landEnvironmental MonitoringMETAL POLLUTION;LAND USE;Pb ISOTOPIC COMPOSITIONS;ANTHROPOGENIC;LANTHANUMIndustrial WastePoaceaesol cultivéplombmétal lourdEdetic Acid0105 earth and related environmental sciencesHydrologyLand useEnvironmental and SocietyEarthworm15. Life on landbiology.organism_classificationANTHROPOGENICpollution du sol[SDE.ES]Environmental Sciences/Environmental and SocietyPedogenesisLead13. Climate actionSoil waterEnvironmental scienceEnvironnement et Société
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ASSESSING TRACE ELEMENT (DIS)EQUILIBRIUM AND THE APPLICATION OF SINGLE ELEMENT THERMOMETERS IN METAMORPHIC ROCKS

2018

Abstract Empirical and experimental calibration of single element solubility thermometers, such as Zr-in-rutile, Zr-in-titanite, Ti-in-zircon, and Ti-in-quartz, within the past 13 years has greatly expanded our ability to assess the pressure and temperature conditions of individual minerals associated with specific textures in metamorphic rocks. Combined with advances in in situ techniques for analyzing trace concentrations, this has led to an increase in the combined use of single element thermometers, geochronometers, and isotope ratios, often simultaneously, in metamorphic minerals. Here we review the calibration and application of single element thermometers at the pressure and temperat…

010504 meteorology & atmospheric sciencesIsotopeMetamorphic rockGeochemistryTrace elementMetamorphismMineralogyGeologyengineering.material010502 geochemistry & geophysicsOverprinting01 natural sciencesPartition coefficientGeochemistry and PetrologyRutileTitaniteengineeringGeology0105 earth and related environmental sciencesTerraneGeological Society of America Abstracts with Programs
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Calculating pressure with elastic geobarometry: A comparison of different elastic solutions with application to a calc-silicate gneiss from the Rhodo…

2020

Abstract Raman elastic geobarometry has increasingly been used complementary to metamorphic phase equilibria to estimate the conditions of recrystallization in metamorphic rocks. The procedure of applying Raman elastic barometry to host-inclusion mineral systems requires several steps that involve various assumptions. One of the most essential assumptions is that the mineral host-inclusion system behaves in an elastic and reversible manner. We discuss the discrepant results obtained by different authors employing different analytical solutions for elasticity and explore the assumptions lying behind each method. Furthermore, we evaluate numerically linear and non-linear elastic solutions and…

010504 meteorology & atmospheric sciencesLithologyMetamorphic rockGeochemistryMineralogyGeology010502 geochemistry & geophysics01 natural sciencesSilicatesymbols.namesakechemistry.chemical_compoundchemistryGeochemistry and PetrologysymbolsEclogiteElasticity (economics)Raman spectroscopyQuartzGeology0105 earth and related environmental sciencesGneissLithos
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The effect of microscale pore structure on matrix diffusion—a site-specific study on tonalite

1997

Abstract The matrix diffusion of non-sorbing tracers was studied in rocks from the Syyry area, Central Finland (SY1). The effect of alteration and weathering on rock matrix porosity and on the available pore space, which affects diffusivity, are discussed. The main rock type in the crystalline bedrock of Syyry is a slightly foliated, gray tonalite with mica gneiss inclusions as well as minor, more mafic inclusions. The total porosity and the spatial porosity distribution and microstructure of the rocks were investigated using infiltration of carbon- 14-methylmethacrylate, electron microscopy and Hg-porosimetry. The laboratory-scale diffusion experiments were performed using (1) the out-leac…

010504 meteorology & atmospheric sciencesMetamorphic rock0207 environmental engineeringMineralogy02 engineering and technologyengineering.material01 natural sciencesFick's laws of diffusionSilicateMatrix (geology)chemistry.chemical_compoundchemistryengineeringEnvironmental ChemistryPlagioclase020701 environmental engineeringPorosityBiotite0105 earth and related environmental sciencesWater Science and TechnologyGneissJournal of Contaminant Hydrology
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Late Palaeoproterozoic depositional age for khondalite protoliths in southern India and tectonic implications

2016

Abstract SHRIMP dating of detrital zircons from garnet–sillimanite–cordierite paragneisses (khondalites) of the Trivandrum Block, southern India, revealed nanometer-scale Pb isotopic inhomogeneity in most grains that we ascribe to annealing processes during ultra-high-temperature metamorphism at ca. 570 Ma. Our age data for zircons from six representative khondalite samples do not document any Neo- or Mesoproterozoic detrital grains, and we conclude from the concordant ages and discordant minimum 207Pb/206Pb ages that the khondalite precursor sediments were deposited more than 2.1 Ga ago and were subsequently intruded by granitoid rocks at ca. 1765–2100 Ma. Some detrital zircons in the khon…

010504 meteorology & atmospheric sciencesMetamorphic rockArcheanGeochemistryMetamorphismGeology010502 geochemistry & geophysics01 natural sciencesDharwar CratonGeochemistry and PetrologyKhondaliteProtolithGeology0105 earth and related environmental sciencesTerraneZirconPrecambrian Research
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Neoproterozoic eclogite- to high-pressure granulite-facies metamorphism in the Mozambique belt of east-central Tanzania: A petrological, geochemical …

2017

Abstract This study investigated Neoproterozoic (Pan-African) eclogite- and high-pressure-granulite (E-HPG) facies rocks from the Mozambique belt of east-central Tanzania, collected close to the town of Ifakara and the adjacent Furua area from different tectonic settings, the Palaeoproterozoic Usagaran and the Neoproterozoic Mozambique belt. The studied rocks are E-HPG facies granite- and diorite-gneisses and a meta-gabbroic rock, which are retrogressed to amphibolite- and greenschist-facies conditions. Four different clockwise P-T paths were constructed. The first P-T path for a granodioritic gneiss displays peak metamorphic conditions at ~ 830 °C and ~ 13.0 kbar. The second P-T path for a…

010504 meteorology & atmospheric sciencesMetamorphic rockGeochemistryMetamorphismGeologyMozambique Belt010502 geochemistry & geophysicsGranulite01 natural sciencesGeochemistry and PetrologyTonianEclogitePetrologyProtolithGeology0105 earth and related environmental sciencesGneissLithos
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