Academic literature on the topic 'Vaches Noires, Falaises des (France)'

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Journal articles on the topic "Vaches Noires, Falaises des (France)"

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Roulland, Thomas, Olivier Maquaire, Stéphane Costa, Vincent Compain, Robert Davidson, and Mohand Medjkane. "Dynamique des falaises des Vaches Noires : analyse diachronique historique et récente à l’aide de documents multi-sources (Normandie, France)." Géomorphologie : relief, processus, environnement 25, no. 1 (2019): 37–55. http://dx.doi.org/10.4000/geomorphologie.12989.

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Wisshak, Max, and Liane Hüne. "The new encrusting microproblematicum <i>Circumpodium enigmaticum</i> and its attachment trace <i>Circumpodichnus serialis</i> from the Middle Jurassic of Normandy (France)." Fossil Record 22, no. 2 (2019): 77–90. http://dx.doi.org/10.5194/fr-22-77-2019.

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Abstract. A single specimen of an enigmatic new attachment etching, together with an unknown calcareous encruster partly preserved in situ, has been identified on a belemnite rostrum from the Marnes de Dives Formation (Callovian, Middle Jurassic) of the Falaises des Vaches Noires in Normandy, France. The trace fossil, here established as the new ichnotaxon Circumpodichnus serialis igen. et isp. n., is a uniserial arrangement of very shallow depressions, oval to fusiform in outline, with peripheral pouches and central pits. The trace maker has a morphology unlike any other known calcareous epib
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Monvoisin, Evariste, Ronan Allain, Eric Buffetaut, and Laurent Picot. "New data on the theropod diversity from the Middle to Late Jurassic of the Vaches Noires cliffs (Normandy, France)." Geodiversitas 44, no. 12 (2022): 385–415. https://doi.org/10.5252/geodiversitas2022v44a12.

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Monvoisin, Evariste, Allain, Ronan, Buffetaut, Eric, Picot, Laurent (2022): New data on the theropod diversity from the Middle to Late Jurassic of the Vaches Noires cliffs (Normandy, France). Geodiversitas 44 (12): 385-415, DOI: 10.5252/geodiversitas2022v44a12
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Buffetaut, Eric, and Jérôme Tabouelle. "Thyreophoran vertebrae from the Callovian (Middle Jurassic) of the Vaches Noires cliffs (Normandy, France), with remarks on the dinosaur assemblage from the Vaches Noires." Comptes Rendus Palevol 18, no. 7 (2019): 891–96. http://dx.doi.org/10.1016/j.crpv.2019.04.009.

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Guilbert, V., R. Antoine, C. Heinkelé, et al. "FUSION OF THERMAL AND VISIBLE POINT CLOUDS : APPLICATION TO THE VACHES NOIRES LANDSLIDE, NORMANDY, FRANCE." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLIII-B2-2020 (August 12, 2020): 227–32. http://dx.doi.org/10.5194/isprs-archives-xliii-b2-2020-227-2020.

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Abstract. In this paper, we present a methodology to fusion 3D visible and thermal infrared (TIR) information on a coastal landslide area located in Normandy, France. A reflex and TIR camera on-board an Unmanned Aerial Vehicle are utilized to generate a 3D visible and a thermal model using Photogrammetry. A Python-written algorithm is then used to associate the thermal scalar on the TIR model to the closest point on the visible point cloud, before applying α-blending to ease the visualization of both data sets. This methodology leads to the generation of an integrated 3D thermo-visible model,
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Roulland, Thomas, Olivier Maquaire, Stéphane Costa, et al. "Seasonal activity quantification of coast badlands by TLS monitoring over five years at the “Vaches Noires” cliffs (Normandy, France)." Geomorphology 400 (March 2022): 108083. http://dx.doi.org/10.1016/j.geomorph.2021.108083.

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Medjkane, M., O. Maquaire, S. Costa, et al. "High-resolution monitoring of complex coastal morphology changes: cross-efficiency of SfM and TLS-based survey (Vaches-Noires cliffs, Normandy, France)." Landslides 15, no. 6 (2018): 1097–108. http://dx.doi.org/10.1007/s10346-017-0942-4.

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Brignon, Arnaud. "Nouvelles données historiques sur les premiers dinosaures trouvés en France." BSGF - Earth Sciences Bulletin 189, no. 1 (2018): 4. http://dx.doi.org/10.1051/bsgf/2018003.

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Cet article passe en revue les premières découvertes de dinosaures faites en France avant que le terme Dinosauria n’ait été introduit par Richard Owen en 1842. En mettant à part les premières découvertes du théropode Streptospondylus altdorfensis faites au XVIIIe siècle par Charles Bacheley dans le Jurassique des Vaches Noires, les principaux résultats démontrés ici sont les suivants (par ordre chronologique) : 1) les premiers restes de dinosaures (dents de théropodes) du Calcaire de Caen (Bathonien) furent collectés par Arcisse de Caumont dans les carrières de Quilly en, ou avant, avril 1826
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Le Mort, Jonas, Jeremy E. Martin, Laurent Picot, and Stéphane Hua. "First description of the most complete Metriorhynchus aff. superciliosus (Thalattosuchia) specimen from the Callovian of the Vaches-Noires cliffs (Normandy, France) and limitations in the classification of Metriorhynchidae." Annales de Paléontologie 108, no. 3 (2022): 102539. http://dx.doi.org/10.1016/j.annpal.2022.102539.

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Hassen, Imen, Cyrille Fauchard, Raphael Antoine, et al. "3D geological modelling of a coastal area: case study of the Vaches Noires Cliffs, Normandy, France." Bulletin of Engineering Geology and the Environment, September 1, 2020. http://dx.doi.org/10.1007/s10064-020-01955-z.

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Dissertations / Theses on the topic "Vaches Noires, Falaises des (France)"

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Kouah, Mohamed Amine Walid. "Μοdélisatiοn numérique des glissements de terrain : de l’initiatiοn à la transitiοn sοlide-fluide des géοmatériaux. : applicatiοn aux falaises des Vaches Νοires (Νοrmandie, France)". Electronic Thesis or Diss., Normandie, 2024. http://www.theses.fr/2024NORMC004.

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En Normandie, les falaises des Vaches Noires constituent un secteur original à la morphologie de badlands, affecté par des processus hydrogravitaires (glissements de terrain, coulées de boue, …) emboités dans l’espace et dans le temps. Dans la phase d’initiation, les géomatériaux sont décrits par des lois de comportement élasto- plastique dans le cadre de la mécanique des sols. Toutefois, lorsque ces matériaux perdent leurs propriétés solides après cette initiation et se transforment en un fluide, leur comportement est décrit par la rhéologie des fluides. C'est le cas des coulées de boue argil
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