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Статті в журналах з теми "Séismes – France":
Manchuel, Kevin, Sylvain Pouliquen, Christophe Vergniault, Pierre Arroucau, Romain Le Roux Mallouf, and Jean-François Ritz. "Quelle place pour l’imagerie sismique dans la caractérisation des failles en domaine intraplaque ?" E3S Web of Conferences 342 (2022): 04002. http://dx.doi.org/10.1051/e3sconf/202234204002.
Missaghieh-Poncet, Justin. "Le déploiement de la géothermie en France et en suisse : vers une redéfinition des usages du sous-sol ?" Écologie & politique N° 68, no. 1 (May 3, 2024): 87–103. http://dx.doi.org/10.3917/ecopo1.068.0087.
Veilleur, Valéry, Johanna Chalonec, Ronny Rosillette, and Laurent Peyras. "Évolutions et perspectives des enjeux territoriaux et des usages liés au barrage de la Manzo." E3S Web of Conferences 346 (2022): 02013. http://dx.doi.org/10.1051/e3sconf/202234602013.
Courboulex, Françoise, Anne-Marie Duval, Anne Deschamps, Antony Lomax, and Christophe Larroque. "Les enseignements du petit séisme de Peille (Alpes-Maritimes, France)." Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science 333, no. 2 (July 2001): 105–12. http://dx.doi.org/10.1016/s1251-8050(01)01615-9.
Vogt, Jean. "Ouragan et séisme (France de l'est, Allemagne et Suisse, 1523 et 1756)." Revue Géographique de l'Est 32, no. 1 (1992): 3–10. http://dx.doi.org/10.3406/rgest.1992.2216.
Gueydan-Turek, Alexandra. "De la sismopoétique de Nina Bouraoui : La « pensée du tremblement » face aux fractures identitaires dans Le jour du séisme (1999)." RELIEF - Revue électronique de littérature française 16, no. 1 (July 8, 2022): 194–209. http://dx.doi.org/10.51777/relief12381.
Duco, Fabien, Jean Pierre Faye, Serge Caperaa, and Eric Reubrez. "Seismic Vulnerability Assessment Using the Instrumentation of an Existing Building." Key Engineering Materials 482 (June 2011): 79–87. http://dx.doi.org/10.4028/www.scientific.net/kem.482.79.
Kerob-Bauchet, B., G. Vesin, D. Résière, and H. Mehdaoui. "Prise en charge des patients haïtiens transférés au CHU de Fort-de-France après le séisme du 12 janvier 2010." Transfusion Clinique et Biologique 17, no. 5-6 (December 2010): 430–31. http://dx.doi.org/10.1016/j.tracli.2010.09.134.
Fayolle, Jacky, and Françoise Milewski. "L'investissement fuit le risque." Revue de l'OFCE 53, no. 2 (June 1, 1995): 5–106. http://dx.doi.org/10.3917/reof.p1995.53n1.0005.
"Séismes en France." Médecine de Catastrophe - Urgences Collectives 4, no. 1 (April 2020): 5–8. http://dx.doi.org/10.1016/j.pxur.2020.03.001.
Дисертації з теми "Séismes – France":
Borchiellini, Serge. "Étude des variations de l'émanation du radon dans le sol et les sources : relations avec la sismicité : application aux Alpes-Maritimes." Nice, 1987. http://www.theses.fr/1987NICE4136.
Chiroiu, Lucian. "Modélisation de dommages consécutifs aux séismes. Extension à d'autres risques naturels." Paris 7, 2004. http://www.theses.fr/2004PA070075.
The work deals with the earthquake loss modelling, before and after an event. First is presented the state of the art of the existing models, such as HAZUS or RISK-UE. Next, capacity curves for different model building types are developed and applied in order to obtain loss scenarios for 2 European sites: Barcelona and Nice. The use of the high resolution satellite imagery for the fast detection, mapping and loss estimation after an earthquake is analysed in the frame of a multidisciplinary approach, combining techniques of remote sensing and earthquake engineering. A multi-hazard intensity scale is presented in the end
Baroux, Emmanuel. "Tectonique active en région à sismicité modérée : le cas de la Provence (France) : apport d'une approche pluridisciplinaire." Paris 11, 2000. http://www.theses.fr/2000PA112076.
Gouache, Corentin. "Générateur stochastique de séismes en contexte de sismicité faible à modérée : des données à l'aléa. Cas de la France métropolitaine." Electronic Thesis or Diss., Université de Lorraine, 2021. http://www.theses.fr/2021LORR0136.
French mainland seismicity is considered as low to moderate due to its remoteness from tectonic plate boundaries. A first consequence is that the origins of its seismicity are harder to understand than in active regions close to tectonic plate boundaries. Another consequence is the lack of available data (earthquakes recorded but also strain rates, active faults...). These two observation make difficult to estimate seismic hazard in low-to-moderate seismic areas. The proposed approach is to generate synthetic earthquakes by combining observation and theoretical knowledge on the seismicity of the studied territory. This generator is based on a three-step scheme: (i) the temporal draw of main shocks, (ii) their spatial draw conditioned by magnitude and finally (iii) the generation of aftershocks they produce. The temporal step needs a recurrence rate. Past seismicity of the whole studied area is analysed thanks to the non-parametric inter event time method in order to obtain this wished recurrence rate. Computing the recurrence rate at the whole territory scale allows to keep the maximum quantity of data, reduce the return periods and so estimate main shock frequencies directly form observed data for each magnitude. An implementation has been developed to overcome the accuracy fall of the inter event time method observed when data are sparse. The spatial step needs a regionalization and a spatial density representing seismicity. The regionalization allows maximum magnitude limitation in space: each region is characterized by an allowed maximal magnitude. Location of a synthetic earthquake with a given magnitude is drawn in the spatial density only within regions that allow this magnitude. Aftershocks are generated around main shocks thanks to the Bath law and the proportion – magnitude distribution of aftershocks. The seismic hazard produced by each of the generated earthquakes (main shocks and aftershocks) is computed thanks to a set of weighted Ground-Motion Prediction Equations. The weights are obtained as function of magnitude and distance thanks to The European ground-motion database RESORCE. Finally, from direct observation of the seismic hazard produced by synthetic earthquakes over one million years, annual probabilities of exceedance can be calculated with ease
Alasset, Pierre-Jean. "Sismotectonique et identification des sources sismiques en domaine à déformation lente : Cas des Pyrénées Occidentales et des Alpes du Nord (France).Le tsunami créé par le séisme de Zemmouri (Mw=6.9,Algérie) du 21 Mai 2003." Université Louis Pasteur (Strasbourg) (1971-2008), 2005. https://publication-theses.unistra.fr/public/theses_doctorat/2005/ALASSET_Pierre-Jean_2005.pdf.
The identification of the active faults in regions of slow deformation is a difficult and necessary task to address the seismic hazard assessment. In France, the active faults at the origin of damaging earthquakes are unknown and we chose to apply an approach which combines the geomorphology, paleoseismology, surface geophysics, historical seismicity and calculation of the source parameters in two seismic zones (the Western Pyrenees and the Alps of Haute-Savoie). 4 earthquakes with Io ≥ VII were selected in each studied zone. The analysis of macroseismic data enables us to assign a magnitude to the selected seismic event, linking intensity and magnitude. Application of the paleoseismological approach helps us identifying the E-W trending Lourdes fault in the Pyrenees with a 50-km long rupture subdivided in 3 sub-segments, and a last earthquake probably between 2918 and 4221 BC, and a slip rate of ~ 0. 2 mm/yr. The fault of Remuaz in the northern Alps presents recent postglacial striations showing left-lateral normal faulting in agreement with the inversion of seismic records of the April 1905 earthquake obtained at the Goettingen station. This ~ 10-km fault length probably participates to the origin of the seismic activity of the region and could have a slip rate of ~ 0. 3 mm/yr. The second part of the thesis concern the earthquake of May 21, 2003, magnitude Mw 6. 9, which has affected the Algerian coast. The earthquake caused an average coastal uplift of ~ 0. 55 m along the epicentral area and a tsunami with waves reaching 1 to 2 meters height that affected the Balearic Islands. The generation and propagation of tsunami was modelled using 5 different seismic sources published in the literature. The different data and other observations collected in the epicentral area show that a shallow source (< 8-km-depth) close to the shoreline with an Mw 6. 9 provides a good fit to the dataset and the field observations
Billard, Alain. "Sismicite et monuments antiques : les ponts et canaux sur les aqueducs romains du bassin méditerranéens." Bordeaux 3, 2006. https://extranet.u-bordeaux-montaigne.fr/memoires/diffusion.php?nnt=2006BOR30005.
The aim of this thesis is to understand how roman architects have conceived canal bridges on aqueducts, to resist to earthquakes and of course to winds. If an architectural model stood out all over the Empire, was often the result of a search of stability against dynamic pressures on these works. Some of them have crossed countries, others have much suffered, from others, nothing but toponymics remains. Beyond anthropic action, why?
Lacan, Pierre. "Activité sismotectonique plio-quaternaire de l'ouest des Pyrénées." Pau, 2008. http://www.theses.fr/2008PAUU3027.
The crustal architecture of the present Pyrenean range leads us to identify four seismotectonic units, from east to west (1) the Eastern Pyrenees (2) the Eastern and (3) Western Central Pyrenees and (4) the Western Pyrenees. These units are affected by two different seismicity patterns. The first mode of deformation is triggered by the relative oblique convergence between the Iberian and European plates whereas the second is a consequence of the isostatic exhumation of the mountain ranges, induced by erosion of the thick under-thrusted Iberian crust. In the Western Central Pyrenees, we show Plio-Pleistocene tectonic activity related to the occurrence of a potential seismogenic source in the Arudy area. We also observe potential active tectonic structures in the Axial Zone of the Pyrenees. These can be attributed to the accommodation of strain triggered by the exhumation of the Axial Zone of the Western Central Pyrenees. Finally, we propose an integrated strain model for the recent tectonic activity of the Western Central Pyrenees. In this area, the right-lateral transpression initiated by the oblique convergence between the Iberian and European plates is competing with vertical deformations triggered by the post tectonic surrection of the Axial Zone
Abdul-Wahed, Mohamad Khir. "Étude de la microsismicité induite à partir des sismogrammes tridirectionnels." Vandoeuvre-les-Nancy, INPL, 2001. http://www.theses.fr/2001INPL583N.
Quenet, Grégory. "Les tremblements de terre en France aux XVIIe et XVIIIe siècles : une histoire sociale du risque." Paris 1, 2001. http://www.theses.fr/2001PA010630.
Voillemont, Jean-Charles. "Caractérisation par micro-sismicité induite des milieux poreux fracturés : modélisations par la méthode des lignes de courant d'un site géothermique HDR (Soultz-sous-Forêts, France)." Vandoeuvre-les-Nancy, INPL, 2003. http://www.theses.fr/2003INPL040N.
Книги з теми "Séismes – France":
Dufour, Olivia. Kerviel, enquête sur un séisme financier: Une catastrophe qui peut se reproduire n'importe où, n'importe quand... Paris]: Eyrolles, 2012.
Частини книг з теми "Séismes – France":
"ANNEXE, LA SISMICITÉ DE LA FRANCE EN QUELQUES PHRASES." In Où sera le prochain séisme ?, 177–82. EDP Sciences, 2020. http://dx.doi.org/10.1051/978-2-7598-2037-5-009.
"ANNEXE, LA SISMICITÉ DE LA FRANCE EN QUELQUES PHRASES." In Où sera le prochain séisme ?, 177–82. EDP Sciences, 2020. http://dx.doi.org/10.1051/978-2-7598-2037-5.c009.
Wimbush, Antonia. "The Four Problems of Nina Bouraoui." In Autofiction, 113–42. Liverpool University Press, 2021. http://dx.doi.org/10.3828/liverpool/9781800859913.003.0005.