Rincón Calero, P. J.Giner Robles, J. L.Vegas, RamónVicente, Gerardo de2016-09-212016-09-211996http://hdl.handle.net/10272/12669The seismicity in the Castilian foreland of the Betic Cordilleras is in accordance with an intraplate compressive stress-field that is characterized by the coexistence of two stress tensors: SHmax N140°-160°E (regional tensor) and SHmax N60°-70°E (secondary tensor). The subsequent intraplate deformation is accommodated by means of dextral strike-slip faults and crustal flexures. The seismic activity seems to be concentrated in some N130°-150°E fault zones in the front of the Alcaraz ArcspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Stress tensorFault plane mechanismsFault population analysisBetic forelandSeismicitySismicidad en el antepaís de las cordilleras Béticas orientales: determinación del tensor de esfuerzos actualSeismicity in the castillan forelandl of de betic cordilleras: neotectonic stress tensor determinationjournal articleopen access