Literatura científica selecionada sobre o tema "Dynamique des tremblements de terre"
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Artigos de revistas sobre o assunto "Dynamique des tremblements de terre"
Peyrat, Sophie, Raúl Madariaga e Kim Bak Olsen. "La dynamique des tremblements de terre vue à travers le séisme de Landers du 28 juin 1992". Comptes Rendus Mécanique 330, n.º 4 (janeiro de 2002): 235–48. http://dx.doi.org/10.1016/s1631-0721(02)01455-9.
Texto completo da fonteSt-Onge, G., J. Leduc, G. Bilodeau, A. de Vernal, R. Devillers, C. Hillaire-Marcel, V. Loucheur, S. Marmen, A. Mucci e D. Zhang. "Caractérisation des sédiments récents du Fjord du Saguenay (Québec) à partir de traceurs physiques, géochimiques, isotopiques et micropaléontologiques". Géographie physique et Quaternaire 53, n.º 3 (2 de outubro de 2002): 339–50. http://dx.doi.org/10.7202/004873ar.
Texto completo da fonteHenrique Cardoso Do Vale e Silva, Alexandre, e Fabrizia Gioppo Nunes. "Técnicas de Geoprocessamento Aplicada à Análise de Padrões Pontuais como uma Contribuição a Cartografia de Zonas Sísmicas no estado de Goiás". Ateliê Geográfico 10, n.º 2 (13 de setembro de 2016): 128. http://dx.doi.org/10.5216/ag.v10i2.36137.
Texto completo da fonteMomot, Jacques. "Les tremblements de terre en Normandie". Études Normandes 50, n.º 3 (2001): 60–68. http://dx.doi.org/10.3406/etnor.2001.1427.
Texto completo da fonteVitaliano, Dorothy B., Bruno Helly e Alex Pollino. "Tremblements de terre: histoire et archéologie". American Journal of Archaeology 91, n.º 1 (janeiro de 1987): 140. http://dx.doi.org/10.2307/505466.
Texto completo da fonteZúñiga, Leonel E. "Un Tsunami en el Caribe Hondureño en 1856 según registros de la Biblioteca Nacional de Francia". Innovare: Revista de ciencia y tecnología 9, n.º 2 (9 de setembro de 2020): 97. http://dx.doi.org/10.5377/innovare.v9i2.10196.
Texto completo da fonteMohammadioun, Bagher. "Les tremblements de terre et la sûreté nucléaire". Revue Générale Nucléaire, n.º 2 (março de 1993): 127–38. http://dx.doi.org/10.1051/rgn/19932127.
Texto completo da fonteLamy, Jérôme. "Surveiller et prévenir : tremblements de terre et promesses satellitaires". Socio, n.º 12 (25 de abril de 2019): 97–114. http://dx.doi.org/10.4000/socio.4569.
Texto completo da fonteSulem, Jean. "Thermodynamique des grands glissements souterrains". Revue Française de Géotechnique, n.º 169 (2021): 6. http://dx.doi.org/10.1051/geotech/2021020.
Texto completo da fonteCroix-Rouge d'El Salvador. "5. La Croix-Rouge, le Croissant-Rouge et les médias Services d'information et médias: un dialogue permanent". Revue Internationale de la Croix-Rouge 72, n.º 783 (junho de 1990): 260–65. http://dx.doi.org/10.1017/s0035336100059530.
Texto completo da fonteTeses / dissertações sobre o assunto "Dynamique des tremblements de terre"
Croissant, Thomas. "Modélisation numérique de l'impact des grands tremblements de terre sur la dynamique des rivières". Thesis, Rennes 1, 2016. http://www.theses.fr/2016REN1S117/document.
Texto completo da fonteIn mountainous areas, intermediate to large earthquakes (Mw > 6) systematically trigger a large number of landslides supplying the fluvial network with massive volumes of sediment. The progressive evacuation of the sediment out of the epicentral area alters river dynamics and may cause hydro-sedimentary hazards in alluvial plains (river avulsion, inundations, bank erosion, ...). The quantification of sediment transfers is critical to better understand landscape evolution on short timescales (i.e. hours to centuries) and improve hazard management in deposition areas. However, the factors controlling the coarse sediment transfers are still poorly known due to a lack of field measurements and adequate numerical models. The aim of this work is thus to study, via numerical modeling, the parameters influencing landslides evacuation, the transport capacity variations at the gorge/alluvial plain transition and the short-term dynamics and hazards of alluvial fans. This work is set up in the context of the West Coast of New Zealand (NZ) which presents a 50% probability to experience a magnitude 8 earthquake in the next 50 years. This problematic has been addressed analytically and via a numerical approach. Using the analytical approach, we demonstrate that the conservation of long-term transport capacity at the bedrock gorge and alluvial plain transition usually implies the channel narrowing in the alluvial part that is generally realized by a transition to a braided system. We identify discharge variability as the dominant factor of alluvial river long term transport capacity compared to riparian vegetation. To explore the role of channel self-organization on coarse sediment transport, we use Eros, a 2D morphodynamic model able to simulate landscape evolution improved by a new 2D hydrodynamic model. Combined with a sediment transport/deposition model and lateral fluxes modeling (bank erosion and transverse deposition), Eros allows for the emergence of diverse alluvial river regimes and geometries (e.g. straight/sinuous and braided channels) as a function of the external forcing experienced by the river (water and sediment fluxes). The application of Eros on natural cases has required the validation and calibration of its principal parameters using analytical solutions and the morphodynamic reproduction of natural systems such as the evolution of the Poerua river in New Zealand following the Mount Adams landslide. In the downstream part of the catchment, the ensemble numerical simulations demonstrate Eros abilities to 1) efficiently predict the morphodynamic evolution of alluvial fans submitted to different scenarios of large sediment supplies and 2) generate probabilistic risk maps. In the upstream part, the results highlight the dominant role of dynamic river narrowing reducing export times of landslide-derived sediments. We define a new law characterizing export times as a function of landslide volume and pre-landslide transport capacity that predicts mean residence times for a M8 earthquake in a mountain range of 5-30 yr, much lower than previous estimations of ~ 100 yr. The numerical approach developed in this work suggests that the study of mountain ranges response to severe landslide disruption can only be addressed with a 2D model able to account for the non-linearities between river flow, channel geometry and sediment transport. The results allow for a better characterization of landscape dynamics at the scale of a seismic cycle and hydro-sedimentary hazards in the short term
Carbonneau, Charles. "Développement d'une base de donnée [i.e. données] expérimentale sur le comportement dynamique des barrages en béton". Sherbrooke : Université de Sherbrooke, 2000.
Encontre o texto completo da fonteLacroix, Maxine. "Analyse des déplacements permanents des barrages en remblai et en enrochement par des méthodes pseudo-dynamiques pour l'est du Canada". Master's thesis, Université Laval, 2016. http://hdl.handle.net/20.500.11794/27129.
Texto completo da fonteMaltais, Pierre-Olivier. "Simulations numériques du comportement de fondations profondes sous sollicitations dynamiques dans deux dépôts quaternaires de l'Est du Canada". Master's thesis, Université Laval, 2012. http://hdl.handle.net/20.500.11794/24750.
Texto completo da fonteZhang, Zezhong. "Stabilité dynamique des versants et effets de site d’origine géomorphologique : simulations numériques et rétro-analyses". Thesis, Paris Sciences et Lettres (ComUE), 2018. http://www.theses.fr/2018PSLEM074/document.
Texto completo da fonteIn this research work, numerical simulations using the finite difference FLAC software (Itasca) were first conducted with a homogeneous linear elastic slope model in order to characterize the acceleration amplification along the slope surface and behind the slope crest, and then to evaluate the topographic effect on the acceleration amplification. The interaction between the frequency of the seismic input motion applied at the base of the model with the slope angle and height has been deeply investigated. It was found that significant changes in the acceleration amplification factor result from variations in the slope angle and height as well as the signal frequency and duration. In addition, it has been shown that the ground motion amplification due to slope topography result from complex coupling effects between the input waves and the reflected waves on the topographic features and is highly controlled by the ratio between the wavelength of the input signal and the slope height.Numerical simulations are based on geotechnical investigations and geotechnical modeling, and it is necessary to validate the results through comparisons between modeling results and field observations. Frequency domain analysis such as spectral density and frequency response are an effective way to understand process characteristics and the various phenomena that cannot be explained in the time domain. For this purpose, a case study at Xishan Park ridge in Zigong in China has been studied. Site amplifications associated with the ground motion produced by the 2008 Wenchuan earthquake have been evaluated using the Standard Spectral Ratio (SSR) technique and root-mean-square acceleration (arms) method in time domain. 2D numerical analysis using finite difference method using the FLAC software (Itasca) has been then performed and results have been compared with monitoring data. The “simulated” peaks of the spectral amplifications are always lower than those derived from the field records. The strong attenuation of input motion at high frequencies highlights the shortcoming that a signal damping ratio does not adequately represent the energy dissipation in numerical simulations. Significant amplifications occurred at high frequencies (>10 Hz) and are considered to result from local specific conditions such as rock fracturing and ridge steps; thus they do not necessarily occur at the top of the hill. Finally, parametric studies were performed with elastic models in terms of various 2D slope geometries and geological layers to characterize the ground motion amplifications. The purpose of the parametric analysis is to understand the role of the geological layer, slope angle and slope height on the ground motion amplification, and thus to estimate if site amplifications could be responsible for the triggering of landslide. Then, the dynamic analysis on the slope model for different seismic magnitudes was performed and a slope failure based on displacement was created to evaluate the Las Colinas slope stability in Salvador. The numerical results clearly showed that site effects can have induced significant ground motion amplifications that contributed to trigger landslides
Zhang, Zezhong. "Stabilité dynamique des versants et effets de site d’origine géomorphologique : simulations numériques et rétro-analyses". Electronic Thesis or Diss., Paris Sciences et Lettres (ComUE), 2018. http://www.theses.fr/2018PSLEM074.
Texto completo da fonteIn this research work, numerical simulations using the finite difference FLAC software (Itasca) were first conducted with a homogeneous linear elastic slope model in order to characterize the acceleration amplification along the slope surface and behind the slope crest, and then to evaluate the topographic effect on the acceleration amplification. The interaction between the frequency of the seismic input motion applied at the base of the model with the slope angle and height has been deeply investigated. It was found that significant changes in the acceleration amplification factor result from variations in the slope angle and height as well as the signal frequency and duration. In addition, it has been shown that the ground motion amplification due to slope topography result from complex coupling effects between the input waves and the reflected waves on the topographic features and is highly controlled by the ratio between the wavelength of the input signal and the slope height.Numerical simulations are based on geotechnical investigations and geotechnical modeling, and it is necessary to validate the results through comparisons between modeling results and field observations. Frequency domain analysis such as spectral density and frequency response are an effective way to understand process characteristics and the various phenomena that cannot be explained in the time domain. For this purpose, a case study at Xishan Park ridge in Zigong in China has been studied. Site amplifications associated with the ground motion produced by the 2008 Wenchuan earthquake have been evaluated using the Standard Spectral Ratio (SSR) technique and root-mean-square acceleration (arms) method in time domain. 2D numerical analysis using finite difference method using the FLAC software (Itasca) has been then performed and results have been compared with monitoring data. The “simulated” peaks of the spectral amplifications are always lower than those derived from the field records. The strong attenuation of input motion at high frequencies highlights the shortcoming that a signal damping ratio does not adequately represent the energy dissipation in numerical simulations. Significant amplifications occurred at high frequencies (>10 Hz) and are considered to result from local specific conditions such as rock fracturing and ridge steps; thus they do not necessarily occur at the top of the hill. Finally, parametric studies were performed with elastic models in terms of various 2D slope geometries and geological layers to characterize the ground motion amplifications. The purpose of the parametric analysis is to understand the role of the geological layer, slope angle and slope height on the ground motion amplification, and thus to estimate if site amplifications could be responsible for the triggering of landslide. Then, the dynamic analysis on the slope model for different seismic magnitudes was performed and a slope failure based on displacement was created to evaluate the Las Colinas slope stability in Salvador. The numerical results clearly showed that site effects can have induced significant ground motion amplifications that contributed to trigger landslides
Al-Gusab, Hussein Ali Hussein. "Modelisation des maisons à ossature en bois et remplissage en terre". Thesis, Université Grenoble Alpes (ComUE), 2018. http://www.theses.fr/2018GREAI027/document.
Texto completo da fonteA simplified finite element model was proposed for the analysis of timber-framed structures with infilling of rocks and clay morter by using hysteretic constitutive models for joints and structural elements. Three different scales were defined for the identification and validation of hysteretic models: connection, shear wall and full-scale building; comparisons of numerical and test results were performed at each scale. The calibrated model allowed assessing the earthquake-resistant performance of a traditional Haitian one-storey house and could be used for the design of a two-storey house
Caracausi, Antonio. "Noble gases as geochemical tracers of Earth's dynamic and evolution". Electronic Thesis or Diss., Université de Lorraine, 2019. http://www.theses.fr/2019LORR0339.
Texto completo da fonteIn my project, I used the nobles gases (He, Ne, Ar, Kr and Xe) to investigate natural processes occurring in different geodynamical contexts (i.e., subduction, continental collision, rifting), showing how the use of the noble gases is fundamental to constrain the origin of volatiles, and to investigate the Earth interior. Furthermore, I also used these volatiles to recognize the processes (water-gas-rock interaction) that occur during the fluids up rise from the Earth’s interior to the atmosphere and quantitatively constrain the extents of these processes. The results of my project are summarized in five main topics: 1) Insights into the degassing history of Earth’s mantle from high precision noble gas analysis of magmatic gas 2) Noble Gas and Carbon Isotope Systematics at the Seemingly Inactive Ciomadul Volcano (Romania): Evidence for Volcanic Degassing 3) Mantle‐Derived Fluids in the East Java Sedimentary Basin, Indonesia 4) Outgassing of Mantle Volatiles in Compressional Tectonic Regime Away From Volcanism: The Role of Continental Delamination 5) Continental degassing of helium in an active tectonic setting (northern Italy): the role of seismicity
Peyrat, Sophie. "Modélisation des tremblements de terre : rupture, rayonnement et inversion". Paris 11, 2001. http://www.theses.fr/2001PA112140.
Texto completo da fonteVoisin, Christophe. "Les tremblements de terre : de l'initiation à l'arrêt de la rupture". Phd thesis, Grenoble 1, 2000. http://tel.archives-ouvertes.fr/tel-00709781.
Texto completo da fonteLivros sobre o assunto "Dynamique des tremblements de terre"
Madariaga, R. Les tremblements de terre. Paris: Éditions du Centre national de la recherche scientifique, 1991.
Encontre o texto completo da fonteFrançoise, Fauchet, ed. Volcans et tremblements de terre. Paris: France loisirs, 1997.
Encontre o texto completo da fonteFiona, Watt. Volcans et tremblements de terre. Londres [i.e. London]: Usborne, 1996.
Encontre o texto completo da fonteDrysdale, J. A. Canadian earthquakes, 1984 =: Tremblements de terre Canadiens, 1984. Ottawa, Canada: Canadian Government Pub. Centre, 1987.
Encontre o texto completo da fonteDufresne-Lamy, Julien. Mon père, ma mère, mes tremblements de terre: Roman. Paris: Belfond, 2020.
Encontre o texto completo da fonteJérôme, Lambert, e Pascal Bernard, eds. Les tremblements de terre en France: Hier, aujourd'hui, demain. Orléans, France: Editions BRGM, 1997.
Encontre o texto completo da fonteMcGuire, Bill. État d'urgence, la Terre en colère : séisme et éruptions volcaniques: La menace tectonique. Paris: Solar, 2003.
Encontre o texto completo da fonteCanada, Royal Society of, ed. Le tremblement de terre de 1663 dans la Nouvelle-France. [S.l: s.n., 1986.
Encontre o texto completo da fonteSismologie: La musique de la Terre. Paris: Hachette, 1997.
Encontre o texto completo da fonteLaurenti, André. Les tremblements de terre des Alpes-Maritimes: Histoire et sensibilisation. Nice: Serre, 1998.
Encontre o texto completo da fonteCapítulos de livros sobre o assunto "Dynamique des tremblements de terre"
KARLIS, Dimitris, e Katerina ORFANOGIANNAKI. "Modèles de régression de Markov pour les séries chronologiques de comptage des séismes". In Méthodes et modèles statistiques pour la sismogenèse, 165–80. ISTE Group, 2023. http://dx.doi.org/10.51926/iste.9037.ch6.
Texto completo da fonteLecoeur, Christelle. "Tremblements de terre". In 1989, hors-champ de l’architecture officielle?: des petits mondes au Grand, 129. École Nationale Supérieure d’Architecture Paris-Malaquais, 2020. http://dx.doi.org/10.3917/acs.dadou.2020.01.0129.
Texto completo da fonteTAŞKIN, Gülşen, Esra ERTEN e Enes Oğuzhan ALATAŞ. "Revue de l’évaluation multitemporelle des dommages dus aux séismes à l’aide d’images satellitaires". In Détection de changements et analyse des séries temporelles d’images 2, 175–246. ISTE Group, 2024. http://dx.doi.org/10.51926/iste.9057.ch5.
Texto completo da fonte"CHAPITRE VI COUPLAGES ET DYNAMIQUE". In Du soleil à la Terre, 253–308. EDP Sciences, 2020. http://dx.doi.org/10.1051/978-2-86883-467-6.c008.
Texto completo da fonteLASOCKI, Stanisław. "Estimation de la densité par noyau en sismologie". In Méthodes et modèles statistiques pour la sismogenèse, 5–31. ISTE Group, 2023. http://dx.doi.org/10.51926/iste.9037.ch1.
Texto completo da fonteSHEBALIN, Peter, e Sergey BARANOV. "Lois statistiques de l’activité post-sismique". In Méthodes et modèles statistiques pour la sismogenèse, 71–114. ISTE Group, 2023. http://dx.doi.org/10.51926/iste.9037.ch3.
Texto completo da fonte"Chapitre 9. Dynamique de la Terre". In La physique du XXe siècle, 155–68. EDP Sciences, 2003. http://dx.doi.org/10.1051/978-2-7598-0209-8.c010.
Texto completo da fonteVincent, Bernard. "Les tremblements de terre en Espagne et au Portugal". In Les catastrophes naturelles dans l’Europe médiévale et moderne, 77–94. Presses universitaires du Midi, 1996. http://dx.doi.org/10.4000/books.pumi.23456.
Texto completo da fonteCONSOLE, Rodolfo, e Roberto CARLUCCIO. "Développement et application de simulateurs de tremblements de terre". In Méthodes et modèles statistiques pour la sismogenèse, 33–70. ISTE Group, 2023. http://dx.doi.org/10.51926/iste.9037.ch2.
Texto completo da fonteDoutreleau, Véronique. "Les tremblements de terre italiens du xiiie au xve siècle". In Les catastrophes naturelles dans l’Europe médiévale et moderne, 223–32. Presses universitaires du Midi, 1996. http://dx.doi.org/10.4000/books.pumi.23506.
Texto completo da fonteTrabalhos de conferências sobre o assunto "Dynamique des tremblements de terre"
Labra Cenitagoya, Ana Isabel. "Neige ardente ou les métamorphoses des éléments dans les littératures maghrébines d'expression française". In XXV Coloquio AFUE. Palabras e imaginarios del agua. Valencia: Universitat Politècnica València, 2016. http://dx.doi.org/10.4995/xxvcoloquioafue.2016.3173.
Texto completo da fonteRelatórios de organizações sobre o assunto "Dynamique des tremblements de terre"
Lamontagne, M. Tremblements de terre de Charlevoix-Kamouraska. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296140.
Texto completo da fonteLamontagne, M. Tremblements de terre: Charlevoix-Kamouraska, Québec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212605.
Texto completo da fonteNadeau, L., M. Lamontagne, P. Brouillette, J. Locat, S. Castonguay e A. Morin. Tremblements de terre et failles de l'astroblème de Charlevoix (Québec). Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328442.
Texto completo da fonteLamontagne, M. Développement d'un système d'alerte précoce pour les tremblements de terre du Québec. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328951.
Texto completo da fonteLamontagne, M. Les dommages dus aux tremblements de terre dans la région de Québec entre 1608 et 2007. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2008. http://dx.doi.org/10.4095/224834.
Texto completo da fonteTurner, B., M. Quat, M. Boiridy, R. Debicki e P. Thurston. Terre dynamique, Grand Sudbury : anciens fonds marins, roche fragmentée par une météorite, sculpture de l'âge glaciaire, fonderie de Grand Sudbury. Natural Resources Canada/CMSS/Information Management, 2015. http://dx.doi.org/10.4095/329901.
Texto completo da fonteAylsworth, J. M. Nouvelles ressources pédagogiques canadiennes par Ressources naturelles Canada pour les tremblements de terre, les glissements de terrain et les tsunamis (plans de cours, cartes et historique des événements) (Janvier 2012). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2012. http://dx.doi.org/10.4095/290240.
Texto completo da fonteLamontagne, M. Caractéristiques des tremblements de terre de la Vallée du Saint-Laurent entre Montréal et Québec et examen de liens possibles avec les travaux de fracturation hydraulique pour les gaz de shale effectués entre 2006 et 2010. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/299646.
Texto completo da fonteLes tremblements de terre. Natural Resources Canada/CMSS/Information Management, 1990. http://dx.doi.org/10.4095/329887.
Texto completo da fonteTremblements de terre au Canada. Natural Resources Canada/CMSS/Information Management, 1989. http://dx.doi.org/10.4095/329814.
Texto completo da fonte