Estudio de una transversal entre la cuenca de Madrid y la Cordillera Ibérica a partir de datos estructurales, sísmicos y gravimétricos

Abstract

An 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 thickness