Добірка наукової літератури з теми "Sismicité naturelle"
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Статті в журналах з теми "Sismicité naturelle"
Camelbeeck, Thierry. "The importance of human-induced earthquakes in the seismicity of stable continental regions." Bulletin de la Société Royale des Sciences de Liège, 2021, 11–21. http://dx.doi.org/10.25518/0037-9565.10641.
Повний текст джерелаДисертації з теми "Sismicité naturelle"
Minetto, Riccardo. "Essaims sismiques : comparaison des séismes naturels et induits." Electronic Thesis or Diss., Université Grenoble Alpes, 2023. http://www.theses.fr/2023GRALU009.
Повний текст джерелаA seismic sequence is a cluster of earthquakes that occur in close spatial and temporal proximity. One type of seismic sequence is a seismic swarm, which is typically characterized by earthquakes whose location changes over time and by the absence of a single, dominant, large earthquake.In this thesis, I investigate the spatio-temporal evolution of natural and induced seismic swarms with the aim of identifying the physical processes that drive them and characterizing the properties of the activated fault systems. More specifically, I focus on three key aspects of the seismic activity: temporal evolution of the seismicity rate, earthquake location and frequency-magnitude distribution. The study focuses on two seismic swarms. The first one, of natural origin, occurred in the Maurienne valley (French Alps) between 2017 and 2019, while the second one was induced by hydraulic fracturing operations at Preston New Road, UK, in 2019. To ensure a high-resolution analysis of these sequences, I first created improved catalogs, which incorporate newly detected events and more accurate magnitudes and hypocenter locations.The migration of earthquakes during the Maurienne swarm suggests that this sequence may have been triggered by a combination of multiple pulses of high-pressure fluids and earthquake-to-earthquake interactions. Additionally, the proportion of small and large events (i.e., the b-value of the Gutenberg-Richter law) varies in space, and this change may be linked to the size of the active fault systems.In addition to the study of the seismic activity, I applied ambient noise interferometry to assess if stress changes during the Maurienne swarm produced detectable variations in seismic wave velocity. The velocity changes appear to be primarily influenced by a seasonal process possibly related to pore pressure variations due to rainfall. However, during the main period of seismic activity, such changes may also be accentuated by the continuous ground shaking resulting from the prolonged occurrence of earthquakes.The Preston New Road sequence is characterized by a seismicity rate and a frequency-magnitude distribution that gradually evolve as fluids are repeatedly injected and the seismogenic volume expands in size. This suggests that the seismic activity during an injection stage depends on the injection history of past stages.The Maurienne and Preston New Road sequences are just two examples of the broader phenomenon of seismic and induced swarms. Nonetheless, these two sequences illustrate that induced and natural swarms can exhibit similar patterns in their spatio-temporal evolution, such as earthquake migration and the dependence of the b-value on the scale of the fault system. This emphasizes the potential of applying the knowledge gained from studying one type of swarm to improve our understanding of the other
Helms, John A. "Aléa sismique naturel et sismicité induite du projet géothermique européen RCS (Roche Chaude Sèche) de Soultz-sous-Forêts (Bas-Rin, France)." Université Louis Pasteur (Strasbourg) (1971-2008), 1996. http://www.theses.fr/1996STR13145.
Повний текст джерелаTary, Jean-Baptiste. "Relations entre fluides et sismicité dans le domaine sous-marin à partir de sismographes de fond de mer : étude de cas en Mer de Marmara et Application au Delta du Niger." Phd thesis, Université de Bretagne occidentale - Brest, 2011. http://tel.archives-ouvertes.fr/tel-00591269.
Повний текст джерелаFradet, 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.
Повний текст джерелаThis 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
Feignier, Bruno. "Comportement à la source de séismes induits : caractérisation géomécanique." Phd thesis, Grenoble 1, 1989. http://tel.archives-ouvertes.fr/tel-00719602.
Повний текст джерелаЗвіти організацій з теми "Sismicité naturelle"
Guidati, Gianfranco, and Domenico Giardini. Synthèse conjointe «Géothermie» du PNR «Energie». Swiss National Science Foundation (SNSF), February 2020. http://dx.doi.org/10.46446/publication_pnr70_pnr71.2020.4.fr.
Повний текст джерела