RT Journal Article
T1 Morfología y tectónica del talud inferior del Golfo de Cádiz
A1 Vázquez Garrido, Juan Tomás
A1 Medialdea Cela, Teresa
A1 Hernández Molina, F.J.
A1 Somoza Losada, Luis
A1 Díaz del Río, Víctor
A1 Vegas, Ramón
A1 León Buendía, Ricardo
A1 Bárcenas, P.
A1 Maestro, Adolfo
A1 Fernández Puga, Mª Carmen
AB Analysis of bathymetric and seismic reflection data allow us to characterize the processes and structures that generate seafloor morphological features in the lower continental slope and the transition to the abyssal plain of the Betic-Rif Margin. Several differences can be stablished in the lower slope and the transition to the Horseshoe and Sena Abyssal Plains. The lower slope in the Horseshoe sector shows an upper convex - lower concave profile and the transition to the abyssal plain is marked by a scarp related to the activity of a main NE-SW reverse fault. Whereas in the Sena sector the lower slope appears as a convex profile and the region boundary with the abyssal plain is determined by the position of the external front of the Allochthonous Betic-Rif Units.
PB Sociedad Geológica de España.
SN 1576-5172
YR 2004
FD 2004
LK https://hdl.handle.net/20.500.14352/52555
UL https://hdl.handle.net/20.500.14352/52555
LA spa
NO Trasferencia Sedimentaria en Talud y Mega-Oligotostroma (TASYO/GADES)
DS Docta Complutense
RD 4 may 2024