%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Mercier de Lépinay, B.
%A Deschamps, A.
%A Klingelhoefer, F.
%A Mazabraud, Y.
%A Delouis, B.
%A Clouard, V.
%A Hello, Yann
%A Crozon, J.
%A Marcaillou, B.
%A Graindorge, D.
%A Vallée, Martin
%A Perrot, J.
%A Bouin, M. P.
%A Saurel, J. M.
%A Charvis, Philippe
%A St-Louis, M.
%T The 2010 Haiti earthquake : a complex fault pattern constrained by seismologic and tectonic observations
%D 2011
%L fdi:010054243
%G ENG
%J Geophysical Research Letters
%@ 0094-8276
%M ISI:000297258500007
%P L22305
%R 10.1029/2011GL049799
%U https://www.documentation.ird.fr/hor/fdi:010054243
%> https://www.documentation.ird.fr/intranet/publi/2011/12/010054243.pdf
%V 38
%W Horizon (IRD)
%X After the January 12, 2010, Haiti earthquake, we deployed a mainly offshore temporary network of seismologic stations around the damaged area. The distribution of the recorded aftershocks, together with morphotectonic observations and mainshock analysis, allow us to constrain a complex fault pattern in the area. Almost all of the aftershocks have a N-S compressive mechanism, and not the expected left-lateral strike-slip mechanism. A first-order slip model of the mainshock shows a N264 degrees E north-dipping plane, with a major left-lateral component and a strong reverse component. As the aftershock distribution is sub-parallel and close to the Enriquillo fault, we assume that although the cause of the catastrophe was not a rupture along the Enriquillo fault, this fault had an important role as a mechanical boundary. The azimuth of the focal planes of the aftershocks are parallel to the north-dipping faults of the Transhaitian Belt, which suggests a triggering of failure on these discontinuities. In the western part, the aftershock distribution reflects the triggering of slip on similar faults, and/or, alternatively, of the south-dipping faults, such the Trois-Baies submarine fault. These observations are in agreement with a model of an oblique collision of an indenter of the oceanic crust of the Southern Peninsula and the sedimentary wedge of the Transhaitian Belt.
%$ 066