RT Journal Article
T1 Depósitos cuaternarios en el Bajo Ebro: características estratigráficas y deposicíonales
T1 Quaternary deposits in the Bajo Ebro: stratigraphic and depositional characteristics
A1 ArasaTuliesa, A.
AB In the Bajo Ebro quaternary deposits different lithostratigraphic units are distinguished. Fluvial facies with tabular character: Ford Gravels, Colada Sandstones and Aldover Poligenic Gravels all with siliceous elastics. Alluvial facies with calcareous elastics: the Aldover Monogenic Gravels. These units are attributed to the lower and middle Quaternary. Other units that constitutes fluvial terraces, whith calcareous monogenic elastics are differenciated by their textural character: Xerta Blocks, Llop Gravels and the Assud Sands; these units are attributed to the Thyrrhenian. The fluvial river basin is filled with the Ebro Muds attributed to Holocene
PB Sociedad Geológica de España
YR 1994
FD 1994
LK http://hdl.handle.net/10272/13986
UL http://hdl.handle.net/10272/13986
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 13 jun 2026