RT Journal Article
T1 Canales arenosos de la Formación Nájera: Características Deposicionales y factores de control
T1 Sandy Channels of the Nájera Formation: Depositional Characteristics and control factors
A1 Molinero Huguet, J.
A1 Colombo Piñol, Ferrán
AB The studied sedimentological section is located in continental tertiary sediments of the western part of the Ebro Basin, and have been interpreted as being generated by braided streams in a general depositional subenvironment corresponding to the external zones of alluvial fans. In this context we found channel deposits with characteristics that are typical of meandering rivers, suggesting that some streams with a sinuous thalweg circulated within this braid plain. The significant agradational pattern shown by these deposits was conditioned by both the lithological characteristics of the bed and the extra sedimentary supply from a local relief which was formed in response to the activity of a blind thrust
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/11822
UL http://hdl.handle.net/10272/11822
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026