Letteratura scientifica selezionata sul tema "Sismicité faible à modérée"
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Articoli di riviste sul tema "Sismicité faible à modérée":
Manchuel, Kevin, Sylvain Pouliquen, Christophe Vergniault, Pierre Arroucau, Romain Le Roux Mallouf e 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.
Leroy, B., F. Louis, C. Niesten e T. Verheecke. "Étude clinique randomisée sur la prévention des douleurs chroniques postchirurgicales dans les prothèses totales de genou". Douleur et Analgésie 31, n. 4 (dicembre 2018): 178–85. http://dx.doi.org/10.3166/dea-2018-0034.
Allereau, Béatrice, e Waddah Sabouni. "Douleur dans les traitements orthodontiques par aligneurs thermoformés". L'Orthodontie Française 88, n. 4 (dicembre 2017): 383–89. http://dx.doi.org/10.1051/orthodfr/2017028.
Barilari, André. "Le bras de fer entre le juge constitutionnel allemand et la banque centrale européenne". Gestion & Finances Publiques, n. 6 (novembre 2020): 98–103. http://dx.doi.org/10.3166/gfp.2020.6.014.
Rouleau, Isabelle, e Pierre-Luc Mallette. "Validité du test des 48 images dans la détection de la simulation des troubles de la mémoire : données de références". Neuropsychologie clinique et appliquée 3, Fall 2019 (2019): 92–104. http://dx.doi.org/10.46278/j.ncacn.20190517.
Confais, Eric, Gérard Cornilleau, Alain Gubian e Catherine Mathieu. "Croissance française à l'horizon 2000 : haut niveau de chômage ou réduction de la durée du travail ?" Revue de l'OFCE 44, n. 2 (1 marzo 1993): 109–54. http://dx.doi.org/10.3917/reof.p1993.44n1.0109.
Al Asgah, N. A., Bashir M. Jarrar e N. T. Taib. "Structure et histochimie des glandes salivaires sublinguales du dromadaire (Camelus dromedaríus)". Revue d’élevage et de médecine vétérinaire des pays tropicaux 43, n. 4 (1 aprile 1990): 519–27. http://dx.doi.org/10.19182/remvt.8783.
Wingert, Aireen, Jennifer Pillay, Dorothy L. Moore, Samantha Guitard, Ben Vandermeer, Michele P. Dyson, Angela Sinilaite, Matthew Tunis e Lisa Hartling. "Fardeau de la maladie chez les nourrissons et les jeunes enfants hospitalisés pour le virus respiratoire syncytial : un examen rapide". Relevé des maladies transmissibles au Canada 47, n. 09 (10 settembre 2021): 420–41. http://dx.doi.org/10.14745/ccdr.v47i09a05f.
Gharbi, M., M. R. Rjeibi e M. A. Darghouth. "Epidémiologie de la theilériose tropicale bovine (infection par Theileria annulata) en Tunisie : une synthèse". Revue d’élevage et de médecine vétérinaire des pays tropicaux 67, n. 4 (2 ottobre 2015): 241. http://dx.doi.org/10.19182/remvt.20567.
Ramdé, Pascal, Pierre Lapointe e Martial Dembélé. "L’appropriation du changement de politiques universitaires par les étudiants en Afrique subsaharienne : le cas de la réforme Licence-Master-Doctorat au Burkina Faso". Comparative and International Education 48, n. 2 (16 giugno 2020): 1–19. http://dx.doi.org/10.5206/cie-eci.v48i2.10789.
Tesi sul tema "Sismicité faible à modérée":
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
Perron, Vincent. "Apport des enregistrements de séismes et de bruit de fond pour l'évaluation site-spécifique de l'aléa sismique en zone de sismicité faible à modérée". Thesis, Université Grenoble Alpes (ComUE), 2017. http://www.theses.fr/2017GREAU020.
Site effects can greatly increase both the duration and the amplitude of the seismic solicitation imposed on structures. 2D-3D site effects induce broadband amplifications that cannot be simulated up to high frequency (>2-4 Hz) due to the limited resolution of the geological, geophysical and/or geotechnical information. Empirical site effect assessment is therefore essential for reliable observations of this complex phenomenon up to high frequency. However, such assessments often require good quality records from many earthquakes that cannot be rapidly obtained in low seismicity areas.This work presents a comparative analysis of these empirical evaluations on two very different sites, the first in a moderate seismicity context (Provence, France) and the second in a very active context (Kefalonia, Greece). For the Provençal site, nearly 500 earthquakes were recorded in only 2½ years thanks to the use of velocimeters. The site attenuation parameter κ_0 could thus be measured both on the acceleration (κ_(0_AS)) and displacement (κ_(0_DS)) spectra. Our results show that the measurement of κ_0 is relatively reliable on rock sites only, mainly due to the too great disturbance by the amplification for sedimentary sites, even for those that are quite stiff. The standard spectral ratio (SSR) approach provides the relative site effects from the numerous weak motion recordings available at sites located in Provence and Kefalonia. The results show a strong epistemic variability due to the lighting induced by the position of the seismic source with respect to the basin. Thus, while a reliable site response estimation is possible from only a few events for 1D geometries, it requires much more earthquakes evenly distributed around the site when the geometry is 2D-3D. The mean SSR results are then compared with those obtained from methods using the ambient noise. As expected, the H/V spectral ratio approach (HVSR) provides only the fundamental frequency for some sites. Conversely, SSR applied to ambient noise (SSRn) shows very similar results to the SSR method up to high frequency, provided that the reference site is taken in the sedimentary basin. Approaches using the noise correlation (coherence and ANIRF) reveal that the transfer function relative to a rock reference site can be estimated at least up to low frequency (<4 Hz). Methods using ambient noise are promising for a rapid evaluation of the site response and its spatial variability (microzoning), even when seismicity is low. Empirical site effects methods are therefore applicable everywhere. They provide an essential complement to numerical approaches, which remain inevitable when the coverage of available earthquakes is not homogeneous or when soils are likely to present non-linear behaviors.These results led us to propose a methodology for the evaluation of the site-specific seismic hazard, which consists of three main stages: (i) adjustment to the rock reference site of the ground motion prediction equations (GMPEs) using, among others, κ_(0_DS); (ii) Reliable evaluation of the SSR transfer function between at least one site in the basin and the reference site (for which the GMPEs were adjusted); (iii) carrying out this assessment from the ANIRF in the less seismically active regions and/or extension to the entire study area with the SSRn. This methodology allows a much better consideration of the site effects (especially 2D-3D) and a significant reduction of the uncertainties in the evaluations of the site-specific seismic hazard. It only required, simultaneous recording of earthquakes on at least two sites equipped with sensible velocimeters, and to carrying out temporary campaign of ambient noise measurements, if necessary
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.
Larroque, C. "Aléa sismique dans une région intraplaque à sismicité modérée : la jonction Alpes - Bassin Ligure". Habilitation à diriger des recherches, Université de Nice Sophia-Antipolis, 2009. http://tel.archives-ouvertes.fr/tel-00453377.
Rapporti di organizzazioni sul tema "Sismicité faible à modérée":
Guidati, Gianfranco, e Domenico Giardini. Synthèse conjointe «Géothermie» du PNR «Energie». Swiss National Science Foundation (SNSF), febbraio 2020. http://dx.doi.org/10.46446/publication_pnr70_pnr71.2020.4.fr.