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La Cuenca de Los Cameros, situada en el sector NW de la Cadena Ibérica, contiene una potente serie sedimentaria (hasta 9000 m) de carácter fundamentalmente continental y de edad Jurásico terminal-Cretácico inferior, que se depositó en un régimen[...]texto impreso
Omodeo Salé, S. ; Ondrak, R. ; Arribas Mocoroa, José ; Mas Mayoral, José Ramón ; Guimera, J. ; Martinez, L. | Wiley | 2019-04The Mesozoic Cameros Basin, northern Spain, was inverted during the Cenozoic Alpine orogeny when the Tithonian – Upper Cretaceous sedimentary fill was uplifted and partially eroded. Tar sandstones outcropping in the southern part of the basin an[...]texto impreso
Gallart Muset, Josep ; Salas, Ramón ; Guimera, J. ; Mas Mayoral, José Ramón ; Díaz, J. ; Ruiz, M. | Sociedad Geológica de España. | 2004As a result of the Eurasian and African plates convergence, Tertiary intraplate deformation of the Iberian plate gave rise to the basement-involved thrust-system of the Iberian Chain. Subsequently, a crustal thickening beneath the Iberian Chain [...]texto impreso
Guimera, J. ; Salas, Ramón ; Mas Mayoral, José Ramón ; Martín Closas, C. ; Meléndez Hevia, Alfonso ; Alonso, A. | Sociedad Geológica de España. | 2000The 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 inv[...]
