RT Journal Article
T1 Los campos de ondas de arena en la Plataforma Continental del Golfo de Cádiz entre Chipiona y Zahara de los Atunes
T1 Sand waves fields over the Continental Shelf of the Gulf of Cadiz between Chipiona and Zahara de los Atunes
A1 Lobo, Francisco J.
A1 Hernández Molina, F. Javier
A1 Maldonado, Andrés
A1 Rodero, J.
AB The analysis o f the seafloor g éom orpholo gie features In the c o n tin e n ta l s h e lf o f the C u lf o f Cadiz with high resolution seismic profiles reveals a well defined distribution pattern of bedforms controlled by the morphology and the hidrodynamic of the area. Three zones are differentiated according to the bedform types and the hidrodynamic processes: a) a northern, shallow submarine zone at 30 m depth situated between ConiI and Barbate (Barbate ridge), where sand waves migrate towards the SE; b) a southern zone southward of the Barbate ridge, where sand waves migrate towards the NW, and c) the infralittoral-inner shelf between Coni! and Cadiz Bay, where sand waves migrate towards the SE and also are influenced by the waves action
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/12195
UL http://hdl.handle.net/10272/12195
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026