Bejar, M.Herráiz, E.Martínez Díaz, J. J.López, C.Capote, RamónTsige, Meaza2014-07-312014-07-312005http://hdl.handle.net/10272/8670This work analyzes the geological source of the Mw 4.8 February 4 2002, Gérgal earthquake. The interpretation of local geological data, the relocation of the aftershocks sequence using a local velocity model, the focal mechanism calculation and the interferometric study of the area using RADAR images give evidences that support a tensional stress source with a rupture plane oriented NW-SE to NNE-SSWspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Focal mechanismRADAR interferometryGergalInterpretación sismotectónica de la serie sísmica de Gérgal (2002, Mw 4.8) mediante datos sismológicos y de interferometría de RADAR (INSAR)Seismotectonic interpretation of the 2002 Mw 4.8 Gérgal seismic sequence using seismological data and radar interferometry (INSAR)journal articleopen access