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Artykuły w czasopismach na temat "Ubaye swarms"
Thouvenot, F., L. Jenatton, D. Scafidi, C. Turino, B. Potin i G. Ferretti. "Encore Ubaye: Earthquake Swarms, Foreshocks, and Aftershocks in the Southern French Alps". Bulletin of the Seismological Society of America 106, nr 5 (13.09.2016): 2244–57. http://dx.doi.org/10.1785/0120150249.
Pełny tekst źródłaFojtíková, Lucia, i Václav Vavryčuk. "Tectonic stress regime in the 2003–2004 and 2012–2015 earthquake swarms in the Ubaye Valley, French Alps". Pure and Applied Geophysics 175, nr 6 (9.02.2018): 1997–2008. http://dx.doi.org/10.1007/s00024-018-1792-2.
Pełny tekst źródłaFojtíková, Lucia, i Václav Vavryčuk. "Correction to: Tectonic Stress Regime in the 2003–2004 and 2012–2015 Earthquake Swarms in the Ubaye Valley, French Alps". Pure and Applied Geophysics 176, nr 1 (styczeń 2019): 525. http://dx.doi.org/10.1007/s00024-018-2068-6.
Pełny tekst źródłaDe Barros, Louis, Marion Baques, Maxime Godano, Agnès Helmstetter, Anne Deschamps, Christophe Larroque i Francoise Courboulex. "Fluid‐Induced Swarms and Coseismic Stress Transfer: A Dual Process Highlighted in the Aftershock Sequence of the 7 April 2014 Earthquake (Ml 4.8, Ubaye, France)". Journal of Geophysical Research: Solid Earth 124, nr 4 (kwiecień 2019): 3918–32. http://dx.doi.org/10.1029/2018jb017226.
Pełny tekst źródłaDuverger, Clara, Gilles Mazet-Roux, Laurent Bollinger, Aurélie Guilhem Trilla, Amaury Vallage, Bruno Hernandez i Yves Cansi. "A decade of seismicity in metropolitan France (2010–2019): the CEA/LDG methodologies and observations". BSGF - Earth Sciences Bulletin 192 (2021): 25. http://dx.doi.org/10.1051/bsgf/2021014.
Pełny tekst źródłaLeclère, Henri, Guillaume Daniel, Olivier Fabbri, Frédéric Cappa i François Thouvenot. "Tracking fluid pressure buildup from focal mechanisms during the 2003-2004 Ubaye seismic swarm, France". Journal of Geophysical Research: Solid Earth 118, nr 8 (sierpień 2013): 4461–76. http://dx.doi.org/10.1002/jgrb.50297.
Pełny tekst źródłaBaques, Marion, Louis De Barros, Clara Duverger, Hervé Jomard, Maxime Godano, Françoise Courboulex i Christophe Larroque. "Seismic activity in the Ubaye Region (French Alps): a specific behaviour highlighted by mainshocks and swarm sequences". Comptes Rendus. Géoscience 353, S1 (8.09.2021): 1–25. http://dx.doi.org/10.5802/crgeos.76.
Pełny tekst źródłaBaques, Marion, Louis De Barros, Maxime Godano, Clara Duverger i Hervé Jomard. "Swarms and mainshock-aftershocks sequences are both triggered by fluids in the Ubaye Region (Western Alps)". Geophysical Journal International, 11.07.2023. http://dx.doi.org/10.1093/gji/ggad280.
Pełny tekst źródłaJenatton, Liliane, Robert Guiguet, François Thouvenot i Nicolas Daix. "The 16,000-event 2003–2004 earthquake swarm in Ubaye (French Alps)". Journal of Geophysical Research 112, B11 (7.11.2007). http://dx.doi.org/10.1029/2006jb004878.
Pełny tekst źródłaDaniel, G., E. Prono, F. Renard, F. Thouvenot, S. Hainzl, D. Marsan, A. Helmstetter i in. "Changes in effective stress during the 2003–2004 Ubaye seismic swarm, France". Journal of Geophysical Research 116, B1 (29.01.2011). http://dx.doi.org/10.1029/2010jb007551.
Pełny tekst źródłaRozprawy doktorskie na temat "Ubaye swarms"
Leclère, Henri. "Comportement sismo-mécanique des failles crustales et interactions fluides-séismes : Une étude de la région de l'Ubaye (Alpes du sud) combinant sismologie, géologie structurale, pétrophysique et modélisation numérique". Electronic Thesis or Diss., Besançon, 2012. http://www.theses.fr/2012BESA2044.
Pełny tekst źródłaThis work adresses the behavior of faults in the upper continental crust under static conditions and moreparticularly the effect of fluid overpressures on fault reactivation and earthquake triggering. In order toreach this goal, an analysis combining seismology, structural geology, petrophysics, geochemistry andhydromechanical modeling has been carried out in the Ubaye region (southern French-Italian Alps) wherea seismic swarm related to regional faults exposed in the Argentera basement massif (located furthersouth) occurred in 2003-2004. Focal mechanisms of 74 events from this seismic swarm have beendetermined. Based on these mechanisms and other seismological data and on mechanical modeling basedon the Mohr-Coulomb theory, this study allows to confirm that the seismic activity of the swarm waslinked to the presence of overpressurized fluids and to explain the spatio-temporal evolution ofoverpressures. A hydromechanical model is proposed in order to account for the spatio-temporalevolutions of both seismicity and pore fluid overpressures. The study of an exposure of an Argenteraregional fault combining a structural analysis, petrophysical measurements and a hydromechanicalmodeling has allowed to decipher the hydromechanical behavior of faults at hypocentral depths, and moreparticularly to determine the ability of faults to be compacted and to develop fluid overpressures. Lastly,the initiation of earthquakes at or near the base of the seismogenic zone is explored through geochemicaland mechanical analyses of quartz-chlorite veins formed at the base of the seismogenic zone. Theseresults are then compared with those deduced from the analysis of the Ubaye seismic swarm. This workallows to study the seismo-mechanical behavior of faults and the interactions between faults, fluids andearthquakes across the seismogenic zone. It emphasizes the importance of associating seismological,hydraulic et mechanical analyses in the study of active faults