The 2010 Haiti earthquake: A complex fault pattern constrained by seismologic and tectonic observations

• Published in: Geophysical research letters 2011-11, Vol.38 (22), p.n/a
• Main Authors: Mercier de Lépinay, Bernard, Deschamps, Anne, Klingelhoefer, Frauke, Mazabraud, Yves, Delouis, Bertrand, Clouard, Valérie, Hello, Yann, Crozon, Jacques, Marcaillou, Boris, Graindorge, David, Vallée, Martin, Perrot, Julie, Bouin, Marie-Paule, Saurel, Jean-Marie, Charvis, Philippe, St-Louis, Mildor
• Format: Article
• Language: English
• Subjects: afltershocks; Belts; Boundaries; Continental dynamics; Earth Sciences; Earth, ocean, space; Earthquake damage; Earthquakes; Environmental Sciences; Exact sciences and technology; Fault lines; Faults; Focal plane; Geophysics; Global Changes; Haiti 2010 earthquake; Marine; Oceanic crust; Physics; Plate tectonics; Sciences of the Universe; Seismic activity; Seismic engineering; Seismic phenomena; Seismology
• ISSN: 0094-8276; 1944-8007
• DOI: 10.1029/2011GL049799

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°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: the rupture occurred on a wrench fault at the rheologic boundary on top of the under‐thrusting rigid oceanic block, whereas the aftershocks were the result of the relaxation on the hanging wall along pre‐existing discontinuities in the frontal part of the Transhaitian Belt. Key Points Active fault identification for the Jan.12, 2010 Haiti earthquake Ocean Bottom Seismometer ued for aftershocks studies Transpressive mechanism for the Jan.12, 2010 Haiti earthquake