12 SOCQUET ET AL.: GPS MEASUREMENTS TO REFINE INDIA/SUNDA RELATIVE MOTION Ledain, A. Y., et al. (1984), Active Faulting and Tectonics of Burma and Surrounding Regions, Journal of Geophysical Research, 89, 453-472. Lomax, A. (2005), Rapid estimation of rupture extent for large earthquakes: Application to the 2004, M9 Sumatra-Andaman mega-thrust, Geophys. Res. Lett., 32, L10314. McCaffrey, R. (1991), Slip Vectors and Stretching of the Sumatran Fore Arc, Geology, 19, 881-884. McCaffrey, R. (1995), DEFNODE users' gui<strong>de</strong>, (http://www.rpi.edu/~mccafr/<strong>de</strong>fno<strong>de</strong>), edited, Rensselaer Polytechnic Institute, Try, NewYork. McCaffrey, R. (2002), Crustal block rotations and plate coupling, in Plate Boundary Zones, AGU. McCaffrey, R. (2005), Block kinematics of the Pacific - North America plate boundary in the southwestern United States from inversion of GPS, seismological, and geological data, J. Geophys. Res., 110. McCaffrey, R., et al. (2000), Strain partitioning during oblique plate convergence in northern Sumatra: Geo<strong>de</strong>tic and seismologic constraints and numerical mo<strong>de</strong>ling, Journal of Geophysical Research-Solid Earth, 105, 28363-28376. Michel, G. W., et al. (2001), Crustal motion and block behaviour in SE-Asia from GPS measurements, Earth Planet. Sci. Lett., 187, 239-244. Mitchell, A. H. G. (1993), Cretaceous-Cenozoic Tectonic Events in the Western Myanmar (Burma) Assam Region, J. Geol. Soc., 150, 1089-1102. Nielsen, C., et al. (2004), From partial to full strain partitioning along the Indo-Burmese hyper-oblique subduction, Marine Geology, 209, 303-327. Okada, Y. (1985), Surface <strong>de</strong>formation due to shear and tensile faults in a half-space, Bull. Seism. Soc. Am., 75, 1135–1154. Paul, J., et al. (2001), The motion and active <strong>de</strong>formation of India, Geophys. Res. Lett., 28, 647- 650. Peltzer, G., and F. Saucier (1996), Present-day kinematics of Asia <strong>de</strong>rived from geologic fault rates, Journal of Geophysical Research-Solid Earth, 101, 27943-27956. Pivnik, D. A., et al. (1998), Polyphase <strong>de</strong>formation in a fore-arc/back-arc basin, Salin subbasin, Myanmar (Burma), AAPG Bull.-Am. Assoc. Petr. Geol., 82, 1837-1856. Prawirodirdjo, L., et al. (1997), Geo<strong>de</strong>tic observations of interseismic strain segmentation at the Sumatra subduction zone, Geophys. Res. Lett., 24, 2601- 2604. Rangin, C., et al. (1999), Cenozoic pull-apart basins in central Myanmar; the trace of the path of India along the western margin of Sundaland, paper presented at European Union of Geosciences conference; EUG 10, Strasbourg, France, March 28-April 1, 1999. Rao, N. P., and M. R. Kumar (1999), Evi<strong>de</strong>nces for cessation of Indian plate subduction in the Burmese arc region, Geophys. Res. Lett., 26, 3149-3152. Ratschbacher, L., et al. (1996), Cenozoic <strong>de</strong>formation, rotation and stress patterns in eastern Tibet and western Sichuan, China, in The tectonic evolution of Asia, edited by A. Y. H., pp. 227-249. Royer, J. Y., and R. Gordon (1997), The motion and boundary between the Capricorn and Australian plates, Science, 277, 1268-1274. Satyabala, S. (2003), Oblique plate convergence in the Indo-Burma (Myanmar) subduction region, Pure Appl. Geophys., 160, 1611 -1650. Simons, W. J. F., et al. (1999), Observing plate motions in Southeast Asia; geo<strong>de</strong>tic results of the GEODYSSEA Project, Geophys. Res. Lett., 26, 2081-2084. Simons, W. J. F., et al. (submitted), A Deca<strong>de</strong> of GPS Measurements in S.E. Asia: (Re)Defining Sundaland and it's Boundaries, J. Geophys. Res. Simons, W. J. F., et al. (2000), Geodynamics of S.E. Asia; first results of the Sulawesi 1998 GPS campaign; IAG general assembly, IAG general assembly, 121, 271-277. Socquet, A., et al. (2002), Late Cretaceous to Eocene metamorphism of the internal zone of the Indo- Burma range (western Myanmar): geodynamic implications, Comptes Rendus Geoscience, 334, 573-580. Socquet, A., and M. Pubellier (2005), Cenozoic <strong>de</strong>formation in Western Yunnan (China-Myanmar bor<strong>de</strong>r), Journal of Asian Earth Sciences, 24, 495- 515. Tapponnier, P., and P. Molnar (1975), Major strike-slip faulting in China; its significance for Asian tectonics, Seismological Society of America, annual meeting, 7, 425-426. Tapponnier, P., and P. Molnar (1977), Rigid plastic in<strong>de</strong>ntation; the origin of syntaxis in the Himalayan Belt Himalaya; sciences <strong>de</strong> la terre, paper presented at Ecologie et geologie <strong>de</strong> l'Himalaya, Paris, France, Dec. 7-10, 1976.
13 SOCQUET ET AL.: GPS MEASUREMENTS TO REFINE INDIA/SUNDA RELATIVE MOTION Vigny, C., et al. (2002), Migration of seismicity and earthquake interactions monitored by GPS in SE Asia triple junction: Sulawesi, Indonesia, Journal of Geophysical Research-Solid Earth, 107, art. no.- 2231. Vigny, C., et al. (2005), GPS unveils actual impact of the mega thrust earthquake in SE Asia, Nature, 24, 495-515. Vigny, C., et al. (2003), Present day crustal <strong>de</strong>formation around Sagaing fault, Myanmar, Journal of Geophysical Research-Solid Earth, 108(B11), 2533. Walpersdorf, A., et al. (1998), GPS compared to longterm geologic motion of the north arm of Sulawesi, Earth Planet. Sci. Lett., 159, 47-55. Walpersdorf, A., et al. (1998), Determining the Sula block kinematics in the triple junction area in Indonesia by GPS, Geophysical Journal International, 135, 351-361. Wang, E., and B. C. Burchfiel (1997), Interpretation of Cenozoic tectonics in the right-lateral accommodation zone between the Ailao Shan shear zone and the eastern Himalayan syntaxis, International Geology Review, 39, 191-219. Wang, E., et al. (1998), Late Cenozoic Xianshuihe- Xiaojiang, Red River, and Dali fault systems of southwestern Sichuan and central Yunnan, China, Special Paper - Geological Society of America, 327, 108.
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Thèse en vue d'obtenir le diplôme
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Résumé Depuis une quinzaine d'ann
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écepteur GPS devient un sismograph
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au diamètre de l'enveloppe du nuag
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Figure 3. répétabilités (c'est
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Les domaines d’application a) con
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cours desquels la faille va moins v
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- Y a-t-il un régime permanent ? o
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temps en temps (pour refaire régul
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Conclusion Pour tous les objectifs
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Les vitesses calculées sur la pér
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A cause des progrès des mesures en
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Il est probable que l'on va bientô
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attendre longtemps pour que ce mouv
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Les réseaux GPS en Birmanie et les
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Chargement élastique sur la faille
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à l'échelle de toute la Birmanie
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vitesses observées et modélisées
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