Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/67272
Title: Deformación cortical de las Béticas Orientales mediante GPS y su relación con el terremoto de Lorca
Author: Echeverria Moreno, Ana
Khazaradze, Giorgi
Gárate, Jorge
Asensio Ferreira, Eva
Suriñach Cornet, Emma
Keywords: Sistema de posicionament global
Tectònica de plaques
Serralades Bètiques
Sismologia
Llorca (Múrcia)
Global Positioning System
Plate tectonics
Benéticos Range (Spain)
Seismology
Lorca (Murcia)
Issue Date: 24-Sep-2012
Publisher: Universidad Complutense de Madrid
Abstract: On May 11th of 2011, a seismic series occurred near the city of Lorca (Murcia). The main earthquake of magnitude Mw 5.2 has been attributed to the Alhama de Murcia Fault, one of the most active faults in the SE Iberian Peninsula. We analyzed 15 years GPS survey data from the CuaTeNeo network to obtain the velocity field in the area. The velocities of the stations closest to the Alhama de Murcia Fault show the reverse and strike-slip direction of motion. Stations located on the southeastern side of the fault have higher velocities between (1.4 and 1.8 mm/yr) oriented towards NNW direction, oriented obliquely to the trace of the fault. The calculated focal mechanism of Lorca earthquake matches the kinematics of the fault and the strain rate directions obtained from the CuaTeNeo network GPS measurements. Detailed analysis of the time-series from the continuous GPS station at the city Lorca allows the detection of co-seismic offset of 6 to 7 mm to the North.
Note: Reproducció del document publicat a: http://dx.doi.org/10.5209/rev_FITE2012.v24.40134
It is part of: Física de la Tierra, 2012, vol. 24, p. 113-127
Related resource: http://dx.doi.org/10.5209/rev_FITE2012.v24.40134
URI: http://hdl.handle.net/2445/67272
ISSN: 0214-4557
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

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