@article{10272/7607,
year = {1986},
url = {http://hdl.handle.net/10272/7607},
abstract = {El Alto nivel aluvial, en este sector del litoral de Huelva, es el pri¬mer indicador de la instauración de la red fluvial cuaternaria; con ríos de cursos entrelazados, mayoritariamente, y variaciones locales de tipo meandriforme condicionadas por el paleorrelieve previo.},
abstract = {The upper alluvial level from Hueiva littoral, southern Spain, re¬presents the first indication of a fluvial quaternary environment, with platform and terrace landforms. This deposit lies over the pliocene paleorelief, which shows an alteration phenomenon with laterite pro¬files. The fluvial deposits are mainly braided with channel and bar facies although some meandering sequences may be formed as result of a topographic control.},
publisher = {Institut de Ciències de la Terra "Jaume Almera"},
publisher = {Universidad de Barcelona},
publisher = {Institut de Diagnosi Ambiental i Estudis de l'Aigua},
publisher = {Universidad Autónoma de Barcelona},
publisher = {Consejo Superior de Investigaciones Científicas},
publisher = {Institut Geològic de Catalunya},
title = {Caracteres sedimentológicos y geomorfológicos del Alto Nivel Aluvial cuaternario en el litoral de Huelva},
author = {Pendón Martín, José Gabriel and Rodríguez Vidal, Joaquín},
}