French West Indies) Seismic Aftershock Sequence Observed with Ocean Bottom Seismometers
ARTICLE IN PRESS TECTO-124885; No of Pages 13 Tectonophysics xxx (2010) xxx–xxx Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto The 2004–2005 Les Saintes (French West Indies) seismic aftershock sequence observed with ocean bottom seismometers S. Bazin a,b,c,⁎, N. Feuillet c,d, C. Duclos b,c, W. Crawford b,1, A. Nercessian e, M. Bengoubou-Valérius a,f, F. Beauducel a,e, S.C. Singh b a Observatoire Volcanologique et Sismologique de Guadeloupe, IPGP, 97113 Gourbeyre, Guadeloupe, French West Indies b Géosciences Marines, IPGP, CNRS-INSU, 4 place Jussieu, 75005 Paris, France c Observatoire Volcanologique et Sismologique de Martinique, IPGP, 97250, Fonds Saint-Denis, Martinique, French West Indies d Tectonique et Mécanique de la Lithosphère, IPGP, CNRS-INSU, 4 place Jussieu, 75005 Paris, France e Sismologie, IPGP, CNRS-INSU, 4 place Jussieu, 75005 Paris, France f BRGM Guadeloupe, 97113 Gourbeyre, Guadeloupe, French West Indies article info abstract Article history: On November 21, 2004 an Mw6.3 intraplate earthquake occurred at sea in the French Caribbean. The Received 18 December 2009 aftershock sequence continues to this day and is the most extensive sequence in a French territory in more Received in revised form 12 March 2010 than a century. We recorded aftershocks from day 25 to day 66 of this sequence, using a rapidly-deployed Accepted 9 April 2010 temporary array of ocean bottom seismometers (OBS). We invert P- and S-wave arrivals for a tomographic Available online xxxx velocity model and improve aftershock locations. The velocity model shows anomalies related to tectonic and geologic structures beneath the Les Saintes graben.
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