Martín, S.Vicente, Gerardo de2017-04-042017-04-041995http://hdl.handle.net/10272/13549The paleostress analysis are used here to outline the Alpine deformation of the contact between the Toledo Mountains and the Madrid Basin. This limit results from a system of E-W-trending reverse faults, NW-SE-trending dextral normal strike-slip faults and NNE-SSW-trending sinistral normal strike-slip faultsspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Faults population analysis,Paleostress analysisCuenca de Madrid.Paleoesfuerzos alpinos en el borde suroccidental de la cuenca de Madrid (Montes de Toledo)Alpine paleostress in the South-Western margin of the Madrid basin (Toledo Mountains)journal articleopen access