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Santisteban Navarro, Juan Ignacio ; Mediavilla López, Rosa María ; Martín Serrano, Ángel | Cambridge University Press | 1996The 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[...]texto impreso
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Santisteban Navarro, Juan Ignacio ; Mediavilla López, Rosa María ; Martín Serrano, Ángel | Instituto Nacional de Geología (España). Instituto Jaime Almera | 1991Como resultado de un detallado trabajo cartográfico, estratigráfico y sedimentológico, se propone la división del Paleógeno del sector suroccidental de la Cuenca del Duero en cuatro U.T.S. limitadas por discordancias. Estas D.T.S., que abarcan d[...]texto impreso
López Olmedo, Fabián ; Diaz de Neira, Alberto ; Martín Serrano, Ángel ; Calvo Sorando, José Pedro ; Morales, Jorge ; Peláez Campomanes, Pablo | Sociedad Geológica de España. | 2003The western part of the Madrid Basin shows widespread arkosic deposits of Neogene age characterized by a massive appearance. On the basis of detailed geological mapping, five main stratigraphic units, ranging the Lower and Middle Miocene, have b[...]texto impreso
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Mediavilla López, Rosa María ; Dabrio, Cristino J. ; Martín Serrano, Ángel ; Santisteban Navarro, Juan Ignacio | Cambridge University Press | 1996Vertical aggradation of Neogene fluvial and lacustrine deposits occurred until the Late Neogene in central and northem areas of the Duero Basin, coeval with river incision in the southwestern corner of the basin. The whole basin became exorheic [...]texto impreso
Carral González, M. P. ; Martín Serrano, Ángel ; Santisteban Navarro, Juan Ignacio ; Guerra, A. ; Jiménez Ballesta, R. | Sociedad Geológica de España | 1998El sistema de terrazas del río Guadalquivir, en su primera aproximación al borde de la Meseta, ocupa un segmento de planta rectangular alargada según una de sus principales directrices estructurales. Se identifican tres grupos principales de niv[...]texto impreso
Martín Serrano, Ángel ; Mediavilla López, Rosa María ; Santisteban Navarro, Juan Ignacio | Cambridge University Press | 1996Tertiary deposits of the north-western Iberian Peninsula are heterogeneous because they occur in several morpho-structural positions as isolated and dispersed basins and outerops. The quality of the palaeontological record is usually very poor a[...]texto impreso
Santisteban Navarro, Juan Ignacio ; Martín Serrano, Ángel ; Mediavilla López, Rosa María ; Dabrio, Cristino J. | Cambridge University Press | 1996In the soult western sector of the intracontinetal Duero basin, the post-Hercynian sedimentary record consist of Upper Cretaceous to Quaternary terrestrial sediments. Climates shifted from tropical, with poorly defined seansos (end of Cretaceous[...]texto impreso
The rise of the Central System due to reactivation of late Hercynian fault systems during the Alpine Orogeny directly affected the strcture and stratigraphic framework of the basins nearby that were being filled al the same time. The sedimentary[...]texto impreso
Santisteban Navarro, Juan Ignacio ; Mediavilla López, Rosa María ; Martín Serrano, Ángel ; Dabrio, Cristino J. | Cambridge University Press | 1996The Duero basin occupies a large area in the north-west of the Iberian Península. It has ao approximately quadrangular shape, and three of its four corners are the sites of distinctive sub-basins that extend outwards from the main basic. The dif[...]
