Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/98424
Title: DInSAR coseismic deformation of the May 2011 Mw 5.1 Lorca earthquake, (Southern Spain)
Author: Frontera, T.
Concha, A.
Blanco, P.
Echeverria Moreno, Ana
Goula Suriñach, Xavier
Arbiol, Román
Khazaradze, Giorgi
Pérez, F.
Suriñach Cornet, Emma
Keywords: Geodèsia
Sistema de posicionament global
Escorça terrestre
Tectònica de plaques
Llorca (Múrcia)
Terratrèmols
Geodesy
Global Positioning System
Earth's crust
Plate tectonics
Lorca (Murcia)
Earthquakes
Issue Date: 2-Apr-2012
Publisher: European Geosciences Union (EGU)
Abstract: The coseismic superficial deformation at the region of Lorca (Murcia, southeastern Spain) due to the Mw 5.1 earthquake on 11 May 2011 was characterized by a multidisciplinary team, integrating information from DInSAR, GPS and numerical modelling techniques. Despite the moderate magnitude of the event, quantitative information was obtained from the interferometric study of a pair of TerraSAR-X images. The DinSAR results defined the trace of the fault plane and evidenced uplift of the hanging wall block in agreement with the estimated deformation obtained through an elastic rupture dislocation numerical model. Meanwhile for the footwall block, interferometric results showed that tectonic deformation is masked by an important subsidence related to groundwater extraction previously identified at the area of study. Horizontal crustal deformation rates and velocity vectors,obtained from GPS stations existent at the area, were also coherent with the tectonic setting of the southern margin of the Iberian Peninsula and with the focal mechanism calculated or the Lorca event. The analysis of a continuous GPS site in Lorca showed good agreement with the horizontal N<br>S direction component relative to the numerical model and tectonics of the region. This is the first time at this seismic active area that a multitechnique analysis has been performed immediately after the occurrence of a seismic event, comparing the existing deformation data with a theoretical numerical model based on estimated seismic rupture dislocation.
Note: Reproducció del document publicat a: http://dx.doi.org/10.5194/se-3-111-2012
It is part of: Solid Earth, 2012, vol. 3, p. 111-119
Related resource: http://dx.doi.org/10.5194/se-3-111-2012
URI: http://hdl.handle.net/2445/98424
ISSN: 1869-9510
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

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