RT Journal Article
T1 Evolución sedimentaria de un nuevo sistema turbidftico en el Atlántico sur: el sistema turbidftico de Agadir
T1 Sedimentary evolution of a new turbidite system in tbe South Atlantic: The Agadir turbidite system
A1 Ercilla, Gemma
A1 Alonso, Belén
A1 Pérez Belzuz, F.
A1 Canals, M.
AB The Agadir turbidite system is located on the Morocco continental margin and the Agadir Basin (South Atlantic), and extends from 200 m to 4300 m water depth. Its establishement seems to have occured during the Oligocene, when the Agadir Canyon was formed. This canyon represents the main valley that feeds the turbidite system. The sediments transported through the Agadir Canyon deposited on the Agadir Basin, developing canyon, channel, overbank and depositional lobe deposits. From the Oligocene to present, this turbidite system has migrated laterally being controlled by the (paleo)topography and the local tectonics. Its vertical sedimentary succession is clearly retrogradational. This retrogration is interpreted as the result of the interplay between tectonics and climate
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/12174
UL http://hdl.handle.net/10272/12174
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026