Search results for "GEOLOGIE"

showing 8 items of 8 documents

Structural contacts in subduction complexes and their tectonic significance: the Late Palaeozoic coastal accretionary wedge of central Chile

2007

Understanding the contact between the very low-grade metagreywacke of the Eastern Series and high-pressure metamorphosed schist of the Western Series in the Late Palaeozoic accretionary wedge of central Chile is fundamental for the understanding of the evolution of ancient accretionary wedges. We show the progressive development of structures and finite strain from the least deformed rocks in the eastern part of the Eastern Series of the accretionary wedge to high-pressure schist of the Western Series at the Pacific coast. Upright chevron folds of sedimentary layering are associated with an axial-plane foliation, S1. As the F1 folds became slightly overturned to the west, S1 was folded abou…

010506 paleontologyAccretionary wedgePaleozoicMineralogy010502 geochemistry & geophysics55101 natural sciencesPaleontologyJungpaläozoikumVAE 50014. Life underwaterChile0105 earth and related environmental sciencesVariszisch-herzynische Orogene {Geologie}SubductionSchistChile {Geologie}Geotektonische Entwicklung der Erdkruste {Geologie}GeologyTectonicsShear (geology)38.36AkkretionskeilFoliation (geology)Sedimentary rockVEX 500VAE 812Geology
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Widening of Hydrous Shear Zones During Incipient Eclogitization of Metastable Dry and Rigid Lower Crust—Holsnøy, Western Norway

2021

The partially eclogitized crustal rocks on Holsnøy in the Bergen Arcs, Norway, indicate that eclogitization is caused by the interplay of brittle and ductile deformation promoted by fluid infiltration and fluid‐rock interaction. Eclogitization generated an interconnected network of millimeter‐to‐kilometer‐wide hydrous eclogite‐facies shear zones, which presumably caused transient weakening of the mechanically strong lower crust. To decipher the development of those networks, we combine detailed lithological and structural mapping of two key outcrops with numerical modeling. Both outcrops are largely composed of preserved granulite with minor eclogite‐facies shear zones, thus representing th…

551.8fluid‐induced weakeningCrust551ddc:551.8GeophysicsGeochemistry and PetrologyMetastabilityeclogitization500 Naturwissenschaften und Mathematik::550 Geowissenschaften Geologie::551 Geologie Hydrologie Meteorologieshear zone wideningShear zoneEclogitizationPetrologyGeologyfluid‐rock interaction
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Polyester microplastic fibers affect soil physical properties and erosion as a function of soil type

2021

Microplastics are recognized as a factor of global change contaminating many environmental compartments. Agricultural soils are very likely to receive microplastic contamination and are of particular concern due to their role in food production. Microplastic fibers have already been shown to be able to affect soil properties, but their effect on different soil types is poorly understood. Moreover, limited information is available on how the presence of this pollutant can affect soil water erosion processes, which are extremely important issues in many environments. In the light of this, we performed two experiments (carried out on a microscale) to investigate how the presence of polyester m…

570soil erosion600 Technik Medizin angewandte Wissenschaften::630 Landwirtschaft::630 Landwirtschaft und verwandte Bereiche550Microplastic in soil500 Naturwissenschaften und Mathematik::570 Biowissenschaften; Biologie::570 Biowissenschaften; Biologieerosioncomplex mixtures630Settore AGR/02 - Agronomia E Coltivazioni ErbaceePolyester microplasticsoil typesoil propertiessoil physical properties500 Naturwissenschaften und Mathematik::550 Geowissenschaften Geologie::550 GeowissenschaftenSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Charcoal and stable soil organic matter as indicators of fire frequency, climate and past vegetation in volcanic soils of Mt. Etna, Sicily

2012

Abstract Charcoal fragments in soils are useful to reconstruct past vegetation because the level of preservation is often good enough to determine the tree genus. All forest ecosystems have the potential to burn as a result of naturally occurring or human-induced fires. Forest fires are coupled to climate and are a not-negligible factor of pedogenesis in Mediterranean areas, where they occur frequently. Furthermore, soil organic matter (SOM) is prone to undergo peculiar changes due to forest fires, both in terms of quantity and quality. A soil sequence along an elevational gradient ranging from Mediterranean to subalpine climate zones on slopes of Mt. Etna (Sicily, Italy) was investigated i…

Mediterranean climate010504 meteorology & atmospheric sciencesClimate1904 Earth-Surface ProcessesMediterranean14C dating01 natural sciencesVolcanic soilstable soil organic matterVegetation typeOrganic matter910 Geography & travelCharcoal0105 earth and related environmental sciencesEarth-Surface Processeschemistry.chemical_classificationEcologySoil organic matter04 agricultural and veterinary sciencesVegetation15. Life on land10122 Institute of GeographyPedogenesischemistrySettore AGR/14 - Pedologia13. Climate actionCharcoalvisual_artSoil water551: Geologie und Hydrologie040103 agronomy & agriculturevisual_art.visual_art_medium0401 agriculture forestry and fisheriesEnvironmental sciencePhysical geographyCATENA
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The effect of alternating different water qualities on accumulation and leaching of solutes in a Mediterranean cracking soil

2002

The relevance of bypass flow on water flow, solute or pesticide transport is becoming increasingly recognized. Recent investigations proved that soil salinization may be influenced by bypass flow, i.e. the rapid transport of water and solutes via macropores and/or shrinkage cracks to subsoil and groundwater. This paper explores the role of bypass flow in the process of accumulation and leaching of solutes, as well as of sodium, in a Mediterranean cracking soil irrigated with saline/sodic waters. The results of bypass flow experiments performed on undisturbed soil cores showed that leaching of solutes occurred in concomitance with bypass fluxes when a low salinity solution was alternated wit…

Soil salinitySoil testWater flowcrackingSoil sciencesalinizationcomplex mixturesirrigationclay soilsuitspoelenLeaching (agriculture)salt movementWater Science and TechnologyHydrologymodelLaboratorium voor Bodemkunde en geologieMacroporescheurvormingbypass flowSoil physicsLaboratory of Soil Science and Geologypredictionzware kleigrondenfieldLeaching modelleachingSoil watermiddellandse-zeegebiedverziltingirrigatiehydraulic conductivitymediterranean regionGeologystructured clay soilHydrological Processes
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Delta C-13 pattern of dissolved inorganic carbon in a small granitic catchment: the Strengbach case study

1999

International audience

[CHIM.OTHE] Chemical Sciences/OtherHYDROLOGIE[CHIM.OTHE]Chemical Sciences/OtherGEOLOGIEComputingMilieux_MISCELLANEOUS
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A self-consistent quantification of contributions to differential TGA results of volcanic soil samples

2002

adsorptiemetingLaboratorium voor Bodemkunde en geologieadsorptionvolcanic soilssoil waterLaboratory of Soil Science and Geologymeasurementbodemwatervulkanische gronden
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Fracture Shape and Orientation Contributions to P-Wave Velocity and Anisotropy of Alpine Fault Mylonites

2021

P-wave anisotropy is significant in the mylonitic Alpine Fault shear zone. Mineral- and texture-induced anisotropy are dominant in these rocks but further complicated by the presence of fractures. Electron back-scattered diffraction and synchrotron X-ray microtomography (micro-CT) data are acquired on exhumed schist, protomylonite, mylonite and ultramylonite samples to quantify mineral phases, crystal preferred orientations, microfractures and porosity. The samples are composed of quartz, plagioclase, mica and accessory garnet, and contain 3-5% porosity. Based on the micro-CT data, the representative pore shape has an aspect ratio of 5:2:1. Two numerical models are compared to calculate the…

electron backscattered diffraction550010504 meteorology & atmospheric sciencesScienceMineralogyanisotropyengineering.materialFault (geology)010502 geochemistry & geophysics01 natural sciences500 Naturwissenschaften und Mathematik::550 Geowissenschaften Geologie::550 GeowissenschaftenPlagioclaseAnisotropyQuartz0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryP-wave velocityQSchistsynchrotron X-ray microtomographynumerical modelingAlpine FaultfractureengineeringFracture (geology)General Earth and Planetary SciencesShear zoneGeologyMylonite
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