@article{10272/8755,
year = {2005},
url = {http://hdl.handle.net/10272/8755},
abstract = {The passive margin of the Guadalquivir foreland basin records different stages of evolution during the
tortonian transgression, mainly determinate by sedimentary supply/ accommodation space ratio (A/S ratio,
Cattaneo and Steel, 2003). In a first phase, a high supply from the continental and deltaic systems filled
quickly the low accommodation space and produced an agradational/progradational stacking pattern of
sequences. The second episode is characterized by a change in these conditions, so the passive margin
register a high increase of depth and carbonate facies predominates. Finally, the transgressive maximum is
registered by means of the formation of a condensed level constituted by glauconitic sands and silts. This
transgressive pulse supposed the advance of the shoreline several kilometres towards the foreland},
publisher = {Sociedad Geológica de España},
keywords = {Sea Level Rise},
keywords = {Paleogeography},
keywords = {Tortonian},
keywords = {Guadalquivir Basin},
title = {Respuesta Estratigráfica a la Transgresión Tortoniense en el Margen Pasivo de la Cuenca del Guadalquivir: Datos Preliminares},
title = {Stratigraphical response to the Tortonian Transgression in the Guadalquivir Foreland Margin: A preliminary
approach},
author = {Abad de los Santos, Manuel and Pendón Martín, José Gabriel and Ruiz Muñoz, Francisco and Rodríguez Vidal, Joaquín and López González, Nieves and Mantero, Isabel},
}