@article{10272/13986,
year = {1994},
url = {http://hdl.handle.net/10272/13986},
abstract = {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},
publisher = {Sociedad Geológica de España},
title = {Depósitos cuaternarios en el Bajo Ebro: características estratigráficas y deposicíonales},
title = {Quaternary deposits in the Bajo Ebro: stratigraphic and depositional characteristics},
author = {ArasaTuliesa, A.},
}