2026-06-28T20:32:21Zhttps://docta.ucm.es/rest/oai/request
oai:docta.ucm.es:20.500.14352/1147982025-03-18T14:52:40Zcom_20.500.14352_14col_20.500.14352_18
Docta Complutense author Vicente Muñoz, Gerardo De author González-Casado, J.M. author Muñoz Martín, Alfonso author Giner Robles, Jorge Luis author Rodríguez Pascua, Miguel Angel editor Friend, Peter F. editor Dabrio González, Cristino José 2025-01-16T17:49:08Z 2025-01-16T17:49:08Z 1995 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. 0521461715 10.1017/CBO9780511524851.036 https://hdl.handle.net/20.500.14352/114798 https://doi.org/10.1017/CBO9780511524851.036 https://www.cambridge.org/core/books/abs/tertiary-basins-of-spain/structure-and-tertiary-evolution-of-the-madrid-basin/79E36FE5CBBFA09FB735E53E802A8395 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. eng Structure and alpine evolution of the Madrid basin book part 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