Search results for "Argile"

showing 10 items of 17 documents

Late Cretaceous continental weathering evolution on the southern Atlantic margins of Africa and South America : contributions of a new geochemical tr…

2022

The late Cretaceous records a pronounced decrease in temperatures on a global scale between 90 and 65 million years that marks the first step of the progressive climatic decline ultimately leading to our modern climate mode. This first cooling step is concomitant to a major tectonic uplift of the east South American and west African margins. Relief formation on the African ans South American continent, enhancing continental weathering, can have induced a climatic cooling at a global scale through atmospheric CO2 consumption linked to silicate weathering reactions. The main objective of this project is to explore the potentially determinant impact of this tectonic uplift on the long-term coo…

Altération continentalePaléoclimat[SDE.MCG] Environmental Sciences/Global ChangesMinéralogie des argilesPaleoclimateContinental weatheringGéochimie isotopiqueClay mineralogyCretaceousIsotopic geochemistryCrétacé supérieur
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Lower Aptian climate and recording of the oceanic anoxic event 1a on the terrigenous shelf of the Paris Basin.

2021

Clay minerals[SDU] Sciences of the Universe [physics]d13CorgAptianArgiles à PlicatulesOAE1a
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Astronomical calibration of the Valanginian and the Hauterivian stages (lower cretaceous) : paleoclimatic and paleooceanographic implications

2013

Orbital floating time scales are proposed for the Valanginian Stage and part of the Hauterivian Stage (Early Cretaceous). These are based on the identification of the eccentricity cycles from spectral analyses performed on high-resolution climatic proxies measured on hemipelagic marl-limestone alternations. Five reference sections were analysed in the Vocontian Basin (SE France), spanning the entire Valanginian. A duration of 5,08 myr is proposed for the Valanginian Stage from the identification of the 405-kyr eccentricity cycle. The time frame proposed, combined with available radiometric ages, shows that the mid-Valanginian 13C positive excursion (namely the Weissert Event) occurs prior …

Cyclostratigraphy[SDU.STU]Sciences of the Universe [physics]/Earth SciencesCalibration astronomiqueSusceptibilité magnétiqueÉvénement WeissertCyclostratigraphieMagnetic susceptibilityHauterivian[PHYS.COND.CM-GEN] Physics [physics]/Condensed Matter [cond-mat]/Other [cond-mat.other]Faraoni EventÉvénement Faraoni[SDU.OTHER] Sciences of the Universe [physics]/OtherMilankovitch cyclesHauterivien[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyCortèges argileux[ SDU.OTHER ] Sciences of the Universe [physics]/Other[ SDU.STU ] Sciences of the Universe [physics]/Earth Sciences[ PHYS.COND.CM-GEN ] Physics [physics]/Condensed Matter [cond-mat]/Other [cond-mat.other]Gamma-ray spectrometryAstronomical calibrationClay mineralsValanginien[PHYS.COND.CM-GEN]Physics [physics]/Condensed Matter [cond-mat]/Other [cond-mat.other]Valanginian[SDU.STU] Sciences of the Universe [physics]/Earth Sciences[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/PaleontologyGamma-ray spectral[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology[SDU.OTHER]Sciences of the Universe [physics]/OtherWeissert EventCycles de Milankovitch
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Importance des variations latérales discrètes dans les apports détritiques, observées dans des faciès de rampe sédimentaire riches en matière organiq…

2017

17 pages; International audience; We studied a potential petroleum source rock deposited in a clastic-dominated ramp environment: the Argiles de Châtillon Formation (Kimmeridgian-Tithonian, Boulonnais area, northern France). The formation was deposited along a proximal-distal gradient on this ramp affected by synsedimentary fault movements. A sedimentological, mineralogical and geochemical study was conducted to decipher the distribution patterns of sedimentary parameters along such a depth increase over the ramp. It comes out that smectite distribution unexpectedly mimics the lateral depth evolution despite the good floatability of the mineral. It is also observed that the Argiles de Châti…

Kimméridgien-Tithonien010504 meteorology & atmospheric sciencesSulfideBoulonnaisGeochemistryMineralogy[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesKimmeridgian-TithonianSedimentary depositional environment[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrygéochimieOrganic matterroches mères d'hydrocarbureComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesgeochemistryorganic matterchemistry.chemical_classificationminéraux argileuxlcsh:QE1-996.5Geology15. Life on landSedimentationlcsh:Geologyclay mineralschemistrySource rockClastic rockmatière organique[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphypetroleum source rocksSedimentary rock[SDU.OTHER]Sciences of the Universe [physics]/OtherClay mineralsGeology
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Magnesium silicate hydrate (M-S-H) characterization : temperature, calcium, aluminium and alkali

2017

The various options to store radioactive wastes in deep geological strata considered in France or Switzerland include the use of large volumes of cementitious materials for infrastructure in contact with argillaceous rocks. So-called low-pH binders were developed to minimize disruption to the surrounding rock by the alkaline plume. Studies conducted on the interaction zone between concrete and clay systematically highlighted the formation of magnesium silicate phases including magnesium silicate hydrate (M-S-H) at the interfaces, which can presently be modeled only partially due to incomplete thermodynamic data. The purpose of this study was to characterize these phases in temperature, alum…

Magnesium silicate hydrate[CHIM.ORGA]Chemical Sciences/Organic chemistryAlkali and calcium bindingAdsorption d’alcalins et de calciumChemical compositionPâtes de ciment bas-PHComposition chimiqueArgile[CHIM.ORGA] Chemical Sciences/Organic chemistrySilicate de magnésium hydratéLow-PH cementModélisations thermodynamiquesClayThermodynamic modelling
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Territorial and socio-economic organisation in Le Grand-Pressigny

2012

In and around Le Grand-Pressigny (Indre-et-Loire, France), a petrographic study was implementedon 92 ceramic samples from the Final Neolithic sites of Le Petit-Paulmy and Bergeresse (Abilly).Analyses showed that the sediments used were extracted from local sources: Claise and Creusealluvium, local substrate and loessic silts. Quantitatively, the study showed that almost all the ceramicmaterials in Bergeresse and more than half of those in Le Petit-Paulmy come from the valley of theCreuse. The mineralogical compositions of three samples from Le Petit-Paulmy, including one ofunusual form, indicate sources from an exogenous region, the Massif Central (perhaps the alluviumof the Loire or the Al…

Néolithique finalargileEurope occidentalePotteryPetrographyClaiseapprovisionnementLe Petit-PaulmyIndre-et-LoireLe Grand-PressignyFlintcéramiqueterritoireAbilly[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and PrehistoryPréhistoireFinal NeolithicCentreCeramic raw-materialsourcesBergeresseminéralogieNeolithic culturesLate Neolithicmatière premièreCreuseFrance
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Evolution climatique au Jurassique inférieur (Sinémuriensupérieur) de la zone Nord-Ouest européenne, déduit de laminéralogie des argiles et des isoto…

2021

National audience; L’étude des minéraux argileux et des isotopes stables (carbone) du Sinémuriensupérieur du bassin de Cardigan Bay (forage de Mochras, Pays de Galles) et du bassinde Paris (forage de Montcornet, France) permet de mettre en évidence les conditionsenvironnementales et climatiques dominantes à cette période. Dans les deux bassins,situés à des paléolatitudes proches (30 à 35°N), les assemblages de minéraux argileuxcomprennent des chlorites, des illites, des interstratifiés illite-smectite (IS R1), dessmectites et des kaolinites dans des proportions variables. L'influence de la diagenèsed’enfouissement et de l'authigénèse étant négligeable dans les deux forages, lesminéraux argi…

[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/ClimatologySinémurien[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/GeochemistrypaléoclimatJurassiqueisotopes du carboneargiles[SDU.STU.MI] Sciences of the Universe [physics]/Earth Sciences/Mineralogy[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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Signatures terrigène et volcanique des bassins sédimentaires : implications stratigraphiques et paléoclimatiques

2018

[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatologysédimentation des argilesstratigraphiepaleoclimate[SDU.STU.VO] Sciences of the Universe [physics]/Earth Sciences/Volcanologypaleoenvironmentspaléoclimat[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/Stratigraphystratigraphypaleovolcanismeclay sedimentationpaléoenvironnentspaléovolcanisme
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Conditions d'hydrolyse au cours du Lutétien-Bartonien dans le Bassin parisien : apport des forages d'Ussy-sur-Marne et du Tillet

2021

L’évolution des conditions climatiques du Paléogène a donné lieu à plusieurs synthèses régionales et globales. Le Bassin parisien, qui est l’un des bassins historiques pour la connaissance des dépôts cénozoïques, a été paradoxalement peu étudié du point de vue des paléoclimats. Cela s’explique par des affleurements dispersés, combinés à une grande variation des environnements de dépôts alternant entre continental et marin ouvert, et un calage stratigraphique complexe. Si les reconstitutions de températures sont accessibles par les données floro-faunistiques et isotopiques (δ18O), l’évolution des conditions hydriques et leurs conséquences sur la production et le transport des sédiments terri…

[SDU] Sciences of the Universe [physics]Minéraux argileuxBassin de Parisaltération continentalechemostratigraphieEocène
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Evolution climatique au Jurassique inférieur (Sinémurien supérieur) de la zone Nord-Ouest européenne, déduit de la minéralogie des argiles et des iso…

2021

International audience

[SDU] Sciences of the Universe [physics]Sinémurien[SDU]Sciences of the Universe [physics]paléoclimatJurassiqueisotopes du carboneargilesComputingMilieux_MISCELLANEOUS
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