RT Journal Article
T1 Estructuración sedimentaria de los cuerpos deltaicos holocenos del margen septentrional del mar de Alborán
T1 Sedimentary structuration ofHolocene deltaic bodies in northem Alboran Sea margin
A1 Hernández Molina, F. Javier
A1 Vázquez Garrido, Juan Tomás
A1 Somoza, L.
A1 Rey Salgado, Jorge
AB In three deltaic areas of northem Alboran Sea margin, the different depositional bodies that establish the sedimentary structure of the holocene progradational wedge has been determinated by high resolution seismic profile (3.5 kHz). Four seismic units have been diferenciated: FI seismic unit (a weak one with an oblicuo-progradational reflection configuration), F2 seismic unit (transparent), F3 seismic unit (a weak one with a sigmoidal-oblique reflection configuration), and F4 seismic unit (transparent). Each one is a real little scale depositional sequence in relation to allocyclical processes by high frecuency eustatic variations during the last 6.000 years
PB Sociedad Geológica de España
YR 1993
FD 1993
LK http://hdl.handle.net/10272/14032
UL http://hdl.handle.net/10272/14032
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 2 jun 2026