RT Book, Section
T1 Structure and alpine evolution of the Madrid basin
A1 Vicente Muñoz, Gerardo De
A1 González-Casado, J.M.
A1 Muñoz Martín, Alfonso
A1 Giner Robles, Jorge Luis
A1 Rodríguez Pascua, Miguel Angel
A2 Friend, Peter F.
A2 Dabrio González, Cristino José
AB The Madrid basin is intracratonic and triangular in form, being bounded on its three sides by Tertiary mountain ranges: the Spanish Central System in the north, the Toledo mountains in the south, and the Iberian and Altomira ranges in the east. The Altomira range separates the Loranca basin from the Madrid basin (Fig. 1). Each of these mountain ranges has a different structure and Tertiary geological evolution. The kinematic history of each of these borders of the Madrid basin reflects differences in the transmission of stresses from the active Iberian plate boundaries where the Betic and Pyrenean chains themselves had distinctive kinematic histories.
PB Cambridge University Press
SN 0521461715
YR 1995
FD 1995
LK https://hdl.handle.net/20.500.14352/114798
UL https://hdl.handle.net/20.500.14352/114798
LA eng
NO Structure and alpine evolution of the Madrid basin (1996) De Vicente, G.; González-Casado, J.M.; Muñoz Martín, A.; Giner Robles, J.L. y Rodríguez Pascua, M.A. Tertiary Basins of Spain. Cambridge Univ. Press (P. Friend y C. Dabrio, Eds.), 255-259.
DS Docta Complutense
RD 3 abr 2025