0000000000083848

AUTHOR

Thierry Baudin

showing 2 related works from this author

Analysis of laser shock waves and resulting surface deformations in an Al-Cu-Li aluminium alloy

2012

Abstract Laser shock processing is now a recognized surface treatment for improving fatigue or corrosion behaviour of metallic materials through the generation of a compressive stress field. In turn, the analysis of shock wave propagation is of primary importance to predict numerically morphological and mechanical surface modifications. Considering experimental and numerical analyses of shock wave propagation, and surface deformations induced by single impacts, a 2050 aluminum alloy having different microstructures was investigated under laser-shock loading. In a first step, the evolution of shock wave attenuation and elastic precursor amplitude was correctly reproduced by finite element si…

Shock wavematière Condensée: Science des matériaux [Physique]Materials sciencechocMatériaux [Sciences de l'ingénieur]Acoustics and UltrasonicsField (physics)Constitutive equation02 engineering and technology01 natural sciences[SPI.MAT]Engineering Sciences [physics]/MaterialsResidual stress0103 physical sciencesComposite materialMécanique: Mécanique des matériaux [Sciences de l'ingénieur]010302 applied physicsaluminiumsimulation numérique021001 nanoscience & nanotechnologyCondensed Matter PhysicsMicrostructureFinite element methodSurfaces Coatings and FilmsElectronic Optical and Magnetic MaterialsShock (mechanics)laserAmplitudeSIMULATION0210 nano-technology
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Kinematics, deformation partitioning and late Variscan magmatism in the Agly massif, Eastern Pyrenees, France

2020

International audience; In order to constrain the finite deformation pattern of the Variscan basement of the Agly massif, a detailed structural analysis over the whole Agly massif was performed. Our investigation combined geological mapping, reappraisal of published and unpublished data completed with our own structural work. Results are provided in the form of new tectonic maps and series of regional cross-sections through the Agly massif. At variance from previous studies, we identified three deformation fabrics named D1, D2 and D3. The D1 deformation is only relictual and characterized by a broadly northwest-southeast striking and eastward dipping foliation without any clear mineral and …

010504 meteorology & atmospheric sciencesCrustal thinningPlutonGneiss domeMetamorphism[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysics01 natural sciencesTranspressionLineationPetrologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesVariscan orogengeographygeography.geographical_feature_categorylcsh:QE1-996.5GeologyMassifPlutonismAgly Massiflcsh:GeologySinistral and dextral[SDU]Sciences of the Universe [physics]eastern pyreneesShear zoneGeology
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