RT Journal Article
T1 The Iberian Chain: tertiary inversion of a mesozoic intraplatebasin
A1 Guimerà, J.
A1 Salas, Ramón
A1 Mas Mayoral, José Ramón
A1 Martín Closas, C.
A1 Meléndez Hevia, Alfonso
A1 Alonso, A.
AB The Mesozoic Iberian basin developed inside the Iberian plate in the eastern end of the Tethys sea. As a result of the Tertiary convergence between the Iberian plate with the European and African plates, the Iberian basin was contractionally inverted, giving rise to the Iberian and Catalan Coastal chains and the surrounding Tertiary basins. The Bouguer anomaly map of the area shows that the Iberian Chain has crustal roots which would have produced during the Tertiary contractional period.
PB Sociedad Geológica de España.
SN 1576-5172
YR 2000
FD 2000
LK https://hdl.handle.net/20.500.14352/57958
UL https://hdl.handle.net/20.500.14352/57958
LA spa
DS Docta Complutense
RD 4 abr 2025