Gallart Muset, JosepSalas, RamónGuimerà, J.Mas Mayoral, José RamónDíaz, J.Ruiz, M.2023-06-202023-06-2020041576-5172https://hdl.handle.net/20.500.14352/52517As a result of the Eurasian and African plates convergence, Tertiary intraplate deformation of the Iberian plate gave rise to the basement-involved thrust-system of the Iberian Chain. Subsequently, a crustal thickening beneath the Iberian Chain was produced, as deduced from Bouguer anomaly maps. A very preliminary interpretation of a new seismic profile through the Iberian Chain is presented, which leads us to infer a crustal thickening beneath the central part of the profile, where Moho depths of at least 40 km should be reached.spajournal articlehttp://www.sociedadgeologica.es/publicaciones_geotemas.htmlopen access551.2/.3Seismic profilecrustal thicknessintraplate deformationIberian ChainSismología (Geología)2507.05 Sismología y Prospección Sísmica