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Tectonophysics 493, 3-4 (2010) 244-253
Faulting characteristics of supershear earthquakes
M. Bouchon 1, H. Karabulut 2, M.P. Bouin 3, J. Schmittbuhl 4, M. Vallée 5, R. Archuleta 6, S. Das 7, F. Renard 1, D. Marsan 8
(2010-10-18)

Recent observations of large continental strike-slip earthquakes show that different fault segments may rupture at different speeds and that rupture may propagate faster than the shear wave velocity of surrounding rocks. We report that all the documented occurrences of supershear rupture are associated with faults which have simple geometry. The surface trace of these faults is described in the field or seen on satellite images as remarkably linear, continuous and narrow. Segmentation features along these segments are small or absent and the deformation is highly localized. As theoretically predicted, supershear is clearly associated with Mode II rupture.
1:  Laboratoire de géophysique interne et tectonophysique (LGIT)
CNRS : UMR5559 – Institut de recherche pour le développement [IRD] – LCPC – OSUG – INSU – Université de Savoie – Université Joseph Fourier - Grenoble I
2:  Observatory and Earthquake Research Institute
Bogazicj University
3:  Observatoire Volcanologique de Guadeloupe
Observatoire Volcanologique de Guadeloupe
4:  Centre National de la Recherche Scientifique
Université de Strasbourg
5:  Géoazur (GEOAZUR)
Université Nice Sophia Antipolis [UNS] – CNRS : UMR6526 – Institut de recherche pour le développement [IRD] – Observatoire de la Côte d'Azur – INSU – Université Pierre et Marie Curie [UPMC] - Paris VI
6:  Department of Earth Science
University of California, Santa Barbara
7:  Department of Earth Sciences
University of Oxford
8:  Université de Savoie
Université de Savoie
Sciences of the Universe/Earth Sciences
Earthquake rupture – Rupture velocity – Fault geometry – Earthquake dynamics – Supershear rupture