Academic literature on the topic 'Noyau ductile'

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Journal articles on the topic "Noyau ductile"

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Rivers, Toby, and Walfried Schwerdtner. "Post-peak Evolution of the Muskoka Domain, Western Grenville Province: Ductile Detachment Zone in a Crustal-scale Metamorphic Core Complex." Geoscience Canada 42, no. 4 (2015): 403. http://dx.doi.org/10.12789/geocanj.2015.42.080.

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The Ottawa River Gneiss Complex (ORGC) in the western Grenville Province of Ontario and Quebec is interpreted as the exhumed mid-crustal core of a large metamorphic core complex. This paper concerns the post-peak evolution of the Muskoka domain, the highest structural level in the southern ORGC that is largely composed of amphibolite-facies straight gneiss derived from retrogressed granulite-facies precursors. It is argued that retrogression and high strain occurred during orogenic collapse and that the Muskoka domain acted as the ductile detachment zone between two stronger crustal units, the
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Van Rooyen, Deanne, and Sharon D. Carr. "Deconstructing the Infrastructure: A Complex History of Diachronous Metamorphism and Progressive Deformation during the Late Cretaceous to Eocene in the Thor-Odin–Pinnacles Area of Southeastern British Columbia." Geoscience Canada 43, no. 2 (2016): 103. http://dx.doi.org/10.12789/geocanj.2016.43.097.

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The Thor-Odin dome is a basement-cored tectonothermal culmination in southern British Columbia containing high-grade metamorphic rocks that were polydeformed in the Late Cretaceous to Eocene. The rocks south of the Thor-Odin dome that extend ca. 20 km to the Pinnacles culmination and Whatshan batholith comprise a heterogeneous tract of polydeformed medium- to high-grade metamorphic rocks and host the South Fosthall pluton near the base of the structural section. They lie in the footwall of the Columbia River fault (CRF) zone, a moderately east-dipping, ductile-brittle, normal fault that was ac
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Konstantinovskaya, Elena, Gennady Ivanov, Jean-Louis Feybesse, and Jean-Luc Lescuyer. "Structural Features of the Central Labrador Trough: A Model for Strain Partitioning, Differential Exhumation and Late Normal Faulting in a Thrust Wedge under Oblique Shortening." Geoscience Canada, March 29, 2019, 5–30. http://dx.doi.org/10.12789/geocanj.2019.46.143.

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The west-verging fold and thrust belt of the Central Labrador Trough originated as a part of the New Quebec Orogen from rift inversion as a result of oblique collision and dextral transpression between the Archean Superior craton and the Archean block of the Core Zone during the Trans-Hudson orogeny (1.82−1.77 Ga). The structures associated with dextral transpression are well established in the northern segment of the orogen but not in the central part. We present new field structural observations along the ca. 70 km long W−E Minowean-Romanet transect that include not only elements of thrust t
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Dissertations / Theses on the topic "Noyau ductile"

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Coget, Yann. "Étude du comportement mécanique à l'impact d'une munition à noyau ductile (petits à moyens calibres)." Electronic Thesis or Diss., Université de Lorraine, 2022. http://www.theses.fr/2022LORR0123.

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Le dimensionnement et l'évaluation des gilets pare-balles nécessitent l'utilisation d'essais balistiques expérimentaux. Ces tests permettent de visualiser en situation réelle, les performances balistiques de la protection à savoir une éventuelle perforation et une déflexion de la face arrière pouvant entraîner des traumatismes lésionnels importants. Cette méthode expérimentale est souvent associée à des modèles éléments finis permettant l'étude de configurations nombreuses et complexes (types de matériaux, épaisseurs, types de munitions, etc.) et d'obtenir non seulement des structures optimisé
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Beaumont, Eric. "Caractérisation cyclique d'un acier austénitique 304L pour implémentation comme matériau de noyau d'une diagonale ductile confinée." Master's thesis, Université Laval, 2017. http://hdl.handle.net/20.500.11794/27870.

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La conception parasismique moderne est toujours en évolution afin de trouver des solutions pour améliorer la performance des structures, pendant des évènements tels que les séismes, tout en demeurant une option économique. Les diagonales ductiles confinées (DDC) sont devenus un choix intéressant comme système de résistance aux charges sismiques, en combinant la grande rigidité latérale des cadres à treillis concentriques avec une très bonne capacité de dissipation d’énergie. Toutefois, ce système est enclin à de grandes flèches latérales permanentes, causées par une faible rigidité suivant la
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