Perucha Atienza, María ÁngelesMuñoz Martín, AlfonsoTejero López, RosaBergamín, J. F.2017-03-212017-03-211995http://hdl.handle.net/10272/13489An integrated geophysical and geological study has been carried out along a trasverse extending from the Madrid Basin to the Iberian Range. Geological and seismic reflection data were used as background model for the gravity modeling. Mesozoic cover structure is characterized by thrusts, E dipping, associated with a decollement located in triassic beds. Gravity modeling shows that high-angle faults bound basement blocks. The faults control triassic sediments thicknessspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Madrid basinAltomira RangeLoranca basinStructureSeismicGravityForward modelingEstudio de una transversal entre la cuenca de Madrid y la Cordillera Ibérica a partir de datos estructurales, sísmicos y gravimétricosIntegrated structural, seismic and gravity data study along a trasverse from the Madrid basin to the Iberian Rangejournal articleopen access