Santisteban Navarro, Juan IgnacioMediavilla López, Rosa MaríaMartín Serrano, ÁngelFriend, Peter F.Dabrio, Cristino J.2023-06-202023-06-2019960521461715https://hdl.handle.net/20.500.14352/60509The tectonic activity in the south-western area of the Spanish Northern Meseta (Ciudad Rodrigo and Duero basins) during most of the Tertiary was determined by u transpressive regime that reactivated Hercynian to Late-Hercynian faults. The record of the Alpine Orogeny is complex because the sedimentary record indicates a compresive regime in the sour e areas coeval with the extensionall to transpresive regime indicated by normal or strike-slip faults. This duality is due 10 the geotectonics position of this area between two compressive areas, the Cantabrian Range and the Central System, and the extensional Atlantic margin.engbook parthttp://www.cambridge.org/9780521021982open access551.3.051(460)551.24(460)Alpine tectonicsSpanishDuero BasinsIberian PeninsulaGeología estratigráfica2506.19 Estratigrafía