RT Journal Article
T1 El relleno de paleodolinas en la cuenca del Ebro y sus posibles aportaciones a la evolución geodinámica y ambiental durante el Pleistoceno
T1 The sedimentary filling ofpalaeodolines in the Ebro Basin: possible contributions to the geodynamic andpalaeoenvironmental evolution during the Pleistocene
A1 Luzón, Aránzazu
A1 Pérez García, Antonio
A1 Soriano, María Asunción
A1 Gil, Héctor
A1 Yuste, Alfonso
A1 Pocoví Juan, Andrés
AB The study of the detrital sediments in the Ebro river terraces near Zaragoza has demonstrated that in this area karst is not only an active phenomenon at present but also during the Pleistocene. The Ebro River system had mainly braided features related to a general high water availability and was affected by the development ofdolines. The ana/ys/s ofdolines filling shows synsedimentary deformation linked to dissolution processes but probably also to tectonics. The preliminary mineralógica! study reveals the existence of some differences depending on the terrace age and also its own potential in palaeoenvironmental and source area studies
YR 2010
FD 2010
LK http://hdl.handle.net/10272/7866
UL http://hdl.handle.net/10272/7866
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 14 jul 2026