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dc.contributor.authorMartí, A.
dc.contributor.authorQueralt, P.
dc.contributor.authorLedo, J.J.
dc.contributor.authorMarcuello, A.
dc.contributor.authorAlvarez-Aramberri, J. 
dc.contributor.authorMartínez-Díaz, J.J.
dc.description.abstractThe Lorca Earthquake (11/5/2011, Mw 5.2) stands as the most destructive in Spain over the last 50 years. It was interpreted as having occurred in an intersegment zone of the strike-slip Alhama de Murcia Fault (AMF). Within the research project "Intergeosima", a multi parametric characterization and monitoring of the fault structure is ongoing, with the aim of developing a future Near Fault Observatory (NFO) to improve the understanding of the seismic behaviour of the fault in the short and medium term. In this work we present the preliminary results of a magnetotelluric (MT) survey carried out along the rambla de la Torrecilla (SW of Lorca). A more resistivity area might correspond to the Quaternary units, whereas the conductive areas might delineate the extent of the fault gauge materials. Further analysis and inversion of the data are necessary to obtain a more detailed picture of the extension and geometry below the fault zone.en_US
dc.rightsReconocimiento-NoComercial-CompartirIgual 3.0 Españaen_US
dc.subjectConductive materialsen_US
dc.subjectFault structureen_US
dc.subjectFault zoneen_US
dc.subjectIntersegment zonesen_US
dc.subjectMedium termen_US
dc.subjectNear faulten_US
dc.subjectParametric characterizationen_US
dc.subjectSeismic behaviouren_US
dc.titleMagnetotelluric characterization of the alhama de murcia fault (Eastern Betics) - Preliminary resultsen_US
dc.journal.title22nd European Meeting of Environmental and Engineering Geophysics, Near Surface Geoscience 2016en_US

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Reconocimiento-NoComercial-CompartirIgual 3.0 España
Except where otherwise noted, this item's license is described as Reconocimiento-NoComercial-CompartirIgual 3.0 España