RT Journal Article
T1 A refraction/wide-angle reflection seismic profile through the Iberian Chain: preliminary report
A1 Gallart Muset, Josep
A1 Salas, Ramón
A1 Guimerà, J.
A1 Mas Mayoral, José Ramón
A1 Díaz, J.
A1 Ruiz, M.
AB As 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.
PB Sociedad Geológica de España.
SN 1576-5172
YR 2004
FD 2004
LK https://hdl.handle.net/20.500.14352/52517
UL https://hdl.handle.net/20.500.14352/52517
LA spa
DS Docta Complutense
RD 12 abr 2025