Tesi sul tema "Séismes – France"
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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.
Arroucau, Pierre. "Sismicité du Massif Armoricain : relocalisations et interprétation tectonique". Phd thesis, Université de Nantes, 2006. http://tel.archives-ouvertes.fr/tel-00117056.
Sansorny-Kohrs, Carine. "Modélisation de la source sismique et sommation de petits séismes pour l'évaluation des mouvements forts : application à une meilleure estimation de l'aléa sismique dans le sud-est de la France". Phd thesis, Université de Nice Sophia-Antipolis, 2005. http://tel.archives-ouvertes.fr/tel-00653557.
Kohrs-Sansorny, Carine. "Modélisation de la source sismique et sommation de petits séismes pour l'évaluation des mouvements forts: application à une meilleure estimation de l'aléa sismique dans le sud-est de la France". Phd thesis, Université de Nice Sophia-Antipolis, 2005. http://tel.archives-ouvertes.fr/tel-00011682.
Pour s'affranchir de la connaissance du milieu de propagation, nous utilisons la technique des fonctions de Green empiriques. Les mouvements du sol sont alors reconstruits par la sommation des enregistrements de plusieurs petits séismes décalés dans le temps de manière à reconstituer le processus de rupture du gros séisme. La principale problématique de cette étude est la mise en place d'un schéma de sommation efficace permettant de générer des accélérogrammes réalistes dans le domaine temporel et en bon accord avec les lois d'échelles (loi de similitude et modèle en w-2) dans le domaine fréquentiel.
Grâce à l'intégration de méthodes statistiques, nous évitons les problèmes majeurs rencontrés classiquement dans ce type d'étude. Nous aboutissons finalement à deux nouvelles méthodes de simulations: une méthode purement stochastique nécessitant la connaissance de seulement deux paramètres concernant le séisme cible (moment sismique et chute de contrainte) et une méthode stochasto-cinématique permettant de reproduire certaines propriétés cinématiques de la rupture sismique sur le plan de faille.
Ces deux méthodes sont testées avec succès sur des données réelles (Mexique et Italie). La méthode stochastique est ensuite appliquée pour simuler les mouvements du sol susceptibles d'être produits par deux séismes de magnitude modérée dans la région niçoise: un séisme de magnitude 5.7 à terre (10 km au nord de Nice) et un séisme de magnitude 6.3 en mer (25 km au sud de Nice). Ces simulations mettent en évidence trois points importants: (1) les forts effets d'amplifications sur certains sites à Nice, (2) l'importance des mouvements du sol susceptibles d'être produits par un séisme de magnitude 5.7 à terre et (3) le rôle majeur joué par la valeur de la chute de contrainte du séisme potentiel.
Kaub, Caroline. "Déformation active intraplaque : étude pluridisciplinaire terre-mer du risque sismique en Vendée, à partir du séisme du Marais Breton de 1799 (M6)". Thesis, Brest, 2019. http://www.theses.fr/2019BRES0024/document.
The Vendée department is classified as a level 3 seismic risk zone because of a moderate background seismic activity and a strong historical seismicity dominated by the 1799 January 25th (M6) major event in the MaraisBreton. This earthquake caused local massive damages in Bouin and around Nantes, and its perception area stretched widely in the West of France. Coastal Vendée is located on the French Atlantic coast, south of the SouthArmorican Shear Zone. This area is made of numerous NW-SE trending hercynian inherited structures, reactivated during Mesozoic and Cenozoic times and delimiting holocene coastal marschlands. The main goal of this thesis is to characterize the geometry of potential plio-quaternary active faults in the area by focusing on the Machecoul fault, bounding the Marais Breton and the Baie de Bourgneuf sedimentary basins and potential candidate for the 1799 earthquake. We used a multidisciplinary onshore-offshore approach, including seismology (temporary network), marine geophysics (Chirp and Sparker seismic reflexion, high resolution bathymetry), morphotectonic, gravity, onshore drilling database and historical seismicity.Our results allowed us to analyze and characterize (1) the Machecoul normal faults system structure and geometry in depth, (2) the plio-quaternary depocenters location in Marais Breton and Baie de Bourgneuf in relation with the Machecoul fault system, reaching locally around twenty meters thick, (3) the hydrographic network perturbation and recent incision of the Machecoul fault footwall, probably pliocene aged relief, (4) the microseismic activity of the Machecoul fault. Our data suggest that the plioquaternary sedimentation of the marine and terrestrial basins located in the south of the fault could be controlled by this inherited fault, probably dated from Eocene age.This work confirms the importance of multi-disciplinary approach in the study of faults in low deformation context and provides a body of evidence allowing to connect the Machecoul fault to the rupture of the 1799 Vendée earthquake (M6), historic and reference event in the western part of France given its scale and so its consequences in the more and more densely populated coastal area
De, La Taille Camille. "Évaluation de l’activité tectonique quaternaire des failles du Jura Méridional (France)". Thesis, Université Grenoble Alpes (ComUE), 2015. http://www.theses.fr/2015GREAU029/document.
Inside the Jura Mountains, left-lateral strike-slip faults intersect the geological structures. In its southern part, these faults, from north to south, the Vuache fault, the Culoz fault and the Col du Chat fault, affect a Mesozoic sedimentary coverage distorted of 2 to 3 km thick and may be the basement. This deformation is marked by the existence of a very shallow seismicity.The first major aim of this thesis is to obtain new information about the kinematic of Quaternary faults of the southern Jura. The second aim is to answer to questions about the geometry and the rooting of the structures.To answer these questions, I realized a multidisciplinary study combining subsurface geophysical (electrical resistivity tomography), lacustrine high resolution seismic, the deployment of a seismic network dedicated to the detection of very low magnitude earthquakes, analysis of reprocessed industrial seismic profiles, and field geology (the study of the structure and deformation of Quaternary deposits). We were able to establish that these faults are active in the Quaternary.The Vuache fault is rooted in the basement, has a well-documented historical and instrumental seismicity, and affects in its southern part Quaternary sediments as shown by electrical resistivity profiles and high resolution seismic profiles illustrating the infill of Annecy Lake.The Culoz fault presents a historical and instrumental seismicity emphasizing its roots in the basement. On land, the electrical resistivity profiles illustrate the quaternary activity, in Lake Le Bourget, the fault Culoz presents at depth a flower structure while to the surface in superficial sediments, we could highlight Riedel fractures. On land, the observation of old faulted Quaternary sediments confirms its activity.The Col du Chat fault affects post-Würm filling of Lake Bourget, and seems to be associated with a deep seismicity.The three studied faults, Vuache, Culoz and Col du Chat are faults showing geometric continuity between the crystalline basement and cover. These faults were considered as transfer faults in the Jura, which was itself considered as a chain formed without the involvement of the basement. So, it seems that at present the deformation of Jura involves the basement. We can then follow the hypothesis, that as shown by the analysis of ECORS profile, that the latest strain of the Jura is an out of sequence deformation involving a basement thrust bellow the High Jura chain probably reusing boundary faults of a Carboniferous basin. This basement thrust would be the main potential source of high magnitude earthquakes in the region.Through these methods, lengths and rooting depth faults were determined. For the three faults studied an estimate of the possible moment magnitude was achieved, a Mw earthquake of 6.2 to 7.2 is possible on the Vuache fault, on the Culoz fault an earthquake of 6.4 to 6.7 can occur while as the Col du Chat fault an earthquake of magnitude Mw 5.4 to 6.1 is possible.The studied strike-slip faults have a sliding rate about tenth of a millimeter per year. In view of the in situ stresses measured in the southern Jura, the driving-force of the deformation on these faults cannot be explained only by the rotation of the Adria plate relative to Eurasia. It is therefore possible that present-day deformation is due to this rotation but also to a driving force linked to the chain itself. This driving-force could be the deflexuration of the plate following mass transfer's deglaciation and a slab break-off inducing the current uplift of the axial part of the Alps and a horizontal stress in the external parts of the chain
Fradet, Thibault. "Vulnérabilité et perception face aux tremblements de terre en France, 1650-1850". Thesis, Université Paris-Saclay (ComUE), 2016. http://www.theses.fr/2016SACLV135/document.
This thesis of history is ultimately the improvement of the methodologies of hazard based on macroseismic data in the case ofhistorical earthquakes. To this end, the effort of basic research, as well as the analysis of the vulnerability of societies of the past to natural hazards involves the creation and the use of methodological tools applicable to historical earthquakes (historical criticism, lexicon, and mapping). The thesis consists into two parts at once distinct and indivisible: firstly the old vulnerability to earthquakes, secondly the vulnerability of ancient buildings.Mixing the context of the available documents with a robust and thin archival research allows integrating the behavior of affected ommunities.Selected time-series terminals correspond to the development of the press and the birth of modern science a hand, entering the era of the Industrial Revolution on the other. This choice is also motivated by the limited availability and more complex analysis of the documents for the period preceding the 17th century and the birth of Seismology for the second part of the 19th century.Three case studies (Bigorre, 1660; Manosque, 1708; Entre-Deux-Mers, 1759) allow exploring many leads of research leading to a better apprehension, analysis and interpretation of historical documents by theuse of tools specifically created for this purpose
Drouet, Stéphane. "Analyse des données accélérimétriques pour la caractérisation de l'aléa sismique en France métropolitaine". Toulouse 3, 2006. http://www.theses.fr/2006TOU30062.
The aim of this study is to analyse the vertical structure of the low troposphere during the ESCOMPTE campaign in relation with transport and diffusion of pollutants. This analysis shows the difficulty to define a boundary layer. It allows us to highlight a complexe superposition of several internal boundary layers, particularly near the coast. The study of the layer where pollution may be accumulated or diluted pointed out the fact that pollution is trapped near the surface, close to the coastline under sea-breeze conditions whereas it is advected over the mountains where the boundary layers are deeper. During sea-breeze conditions, the ozone concentration is paradoxically weak near the sources at the coastline (titration). Over the mountains, the strong developments of the boundary layers result in a mixing between the highly polluted low troposphere and the surface which enhances the ozone concentration
Volant, Philippe. "Mécanisme des déformations et aspect fractal de la sismicité induite par l'exploitation d'un gisement d'hydrocarbures (Lacq, France)". Phd thesis, Grenoble 1, 1993. http://tel.archives-ouvertes.fr/tel-00745639.
Lefeuvre, Benjamin. "La lawsonite dans les métasédiments en base de zone sismogénique : géochimie, échelles de migration des fluides et rôle de la déformation dans les Schistes Lustrés". Electronic Thesis or Diss., Sorbonne université, 2020. http://www.theses.fr/2020SORUS214.
In subduction zones, the migration of fluids derived from the dehydration of metasediments has important consequences on the mechanic properties of rocks, hence on seismicity. Geophysical imaging of the velocity of pressure and shear waves shows that fluids are present in large quantities and migrating in the 30-40 km depth range. This range corresponds to the depth at which slow slip events are supposed to take place, and it is currently assumed that fluids play a large part in the onset of these slow slip events. Deformation mechanisms accompanying slow slip events are still debated, as well as the exact role of fluids, which remain enigmatic in their source, origin, volumetric importance together with the scale and the mode of their migration. To better understand how such fluids migrate in subducted metasediments and refine the budget of fluids in this context (from ~150°C-0.3 GPa to 350°C-1.2 GPa), we have studied subunits of the Schistes Lustrés Complex of the Western Alps. Lawsonite (ideally CaAl2Si2O7(OH)4.H2O) is ubiquitous in these rocks, in the schistose matrix as well as in metamorphic veins, attesting to fluid-rock interactions at depth. Lawsonite, a highly hydrated mineral (~12wt.% H2O) is of particular interest as it is known to play a key role in recycling fluids to mantle depths for it is stable up tu ultra-high pressures. This study aims first at defining which reactions allowed lawsonite crystallization to shed light on element transfer at depth. The petrologic study allowed distinguishing several types of lawsonite based on textural, micro-structural and morphologic criteria. Then, a detailed geochemical study of the lawsonite types has been carried out in this study. Results highlight the differences in fluid-rock interactions and their time evolution. The earliest, most abundant lawsonite type shows closed-system crystallization with small equilibrium length-scales (micro- to millimetres) whereas later lawsonite types indicate system opening with increased fluid mobility and element transfer via advection. Observations concur to showing progressive system opening in the Schistes Lustrés via increased fluid mobility. Scales of fluid mobilization remain uncertain and analysis of strontium isotopic ratios will help further constraining the source of fluids and their interactions with the host rock
Denieul, Marylin. "Moment sismique et coda d'ondes crustales". Thesis, Strasbourg, 2014. http://www.theses.fr/2014STRAH015/document.
Accurate magnitude determination is necessary to establish reliable seismicity catalogs in order to assess seismic hazard. The main goal of this PhD is to develop a method for estimating moment magnitude Mw from coda waves applicable to new digital seismograms as well as to old paper records in France. In order to analyze coda waves properties in France, a study of the regional and frequency properties of coda-wave envelopes has been performed. From this spectral analysis of coda waves, we can estimate seismic moment M0 and moment magnitude Mw from digital seismograms but not from paper records for which no frequency filtering is possible. Therefore, in a second step, we have analyzed the coda-waves properties directly in the time domain. We develop an empirical model which fits the coda envelopes of the raw signal and permits to obtain a coda magnitude Mcoda. From the Mcoda/Mw relationship, we determined the moment magnitude directly from the old paper records in France
Chesterman, Adam. "Des prescriptions aux comportements de protection du risque sismique en région Provence-Alpes-Côte d'Azur : développement d'un paradigme substitutif". Thesis, Aix-Marseille, 2015. http://www.theses.fr/2015AIXM3071.
The goal of this research, conducted in the PACA region, was to understand how to lead individuals to adopt earthquake protection behaviour. To this end, we explored the behavioural effects of self-other substitution, and observed actual protection behaviours in a field study. By interpreting self-other substitution in terms of social comparison, the paradigm relies on a distinction between the uncontrollability of an earthquake and the controllability of its consequences. After having activated a central or peripheral element of the social representation of earthquakes, participants are required to evaluate the probability of an earthquake’s effects in a substitutive context, and then the probability of an earthquake in a standard context. Comparative optimism leads participants to declare that the effects of an earthquake are more probable in a substitutive rather than standard context. Furthermore, a cognitive consistency principle seems to lead participants to declare that an earthquake is more likely after having evaluated the probability of its effects in a substitutive rather than standard context. Protection behaviours were measured using the French version of the Earthquake Readiness Scale. Self-declared protection behaviours were more favourable after a substitutive rather than standard answer. However, the effects on actual behaviours are mixed
Nicey, Jérémie. "Le Journal Télévisé en France et en Suède : Mise en parallèle des modèles français et suédois du traitement de l’actualité nationale et internationale". Paris 3, 2008. http://www.theses.fr/2008PA030182.
Sweden and France, countries from Western Europe, share several patterns within media uses. What about information on television, and more precisely about emblematic TV news bulletins ? This PhD thesis is a crossed look at the news coverage in evening bulletins 20 Heures on private TF1 and public service France 2, Rapport on public service SVT1, and Nyheterna on ‘semi-private’ TV4, with the purpose of answering the following question : could Swedish TV news bulletins landscape, marked for a long time by the tradition of public service, serve as a ‘model’ for its French equivalent ? Dimensions and stakes of the research subject are clarified, at first : the method and the selection criteria of both the programme ‘TV news bulletin’ and the corpus (channels, editions and events). TV news bulletin is examined as an international genre, with its markers, its constraints (time and images) and its construction, based on news collection, editorial choices and ‘mise en scène’. Broadcasting of TV news is compared in both countries by analysing the archives of the coverage of three events : the French presidential elections shock (April-May 2002), the assassination of Swedish Foreign affairs Minister Anna Lindh (September 2003), and the Asian tsunami (December 2004). Prospects about channels strategies for news are finally developed. In a public-private competition context, TV news is a communication and performance stake, but suffers erosion with multiple causes and effects
Riahi, Hassen. "Analyse de structures à dimension stochastique élevée : application aux toitures bois sous sollicitation sismique". Phd thesis, Université Blaise Pascal - Clermont-Ferrand II, 2013. http://tel.archives-ouvertes.fr/tel-00881187.
Velescu, Elena. "La représentation des catastrophes naturelles en littérature et peinture dans l’espace culturel franco-allemand entre la deuxième moitié du XVIIIe siècle et le début du XIXe siècle". Thesis, Paris, EPHE, 2015. http://www.theses.fr/2015EPHE4048.
This research aims to report on the relationships created among natural events of high intensity which can be categorized as natural disasters due to their destructive consequences starting with the famous earthquake of Lisbon in 1755 until the mid-nineteenth century, the advent of new technology and science, which created a new relationship between man and nature. This change in catastrophe representation in literature but also in the painting is based on religious, scientific and aestethetic changes, the key elements that we explored in this work. The aim of this dissertation is to analyze the metamorphoses of writing and visual discourse of the above-mentioned period and draw attention to the transition from horror triggered by a catastrophic event to a sensory dimension and fascination caused by the spectacle of natural phenomena. We also examined the symbolism of the motifs attached to the great myths of humanity, such as the Flood, the theme of transgression-punishment-redemption part of the disaster, which generates into a new concept, an object of analysis, reflection and contemplation, which inspires us to see the catastrophic events differently
Vu, Thanh Kien. "Incidence de la torsion sur la résistance sismique de bâtiments courants avec diaphragmes horizontaux rigides. Application aux structures en bois". Phd thesis, Université Blaise Pascal - Clermont-Ferrand II, 2011. http://tel.archives-ouvertes.fr/tel-00697025.
Massin, Frédérick. "Transferts et Stockages Magmatiques au Piton de la Fournaise". Phd thesis, Université de la Réunion, 2009. http://tel.archives-ouvertes.fr/tel-00710063.