Caracterización sedimentaria de facies tempestíticas en barreras arenosas del estuario de Huelva (SO España)
- P. Gómez
- J. Rodríguez Vidal
- M.L. González Regalado
- M.J. Clemente
- L.M. Cáceres
- A. Toscano
- M. Abad
- T. Izquierdo
- F. Ruiz
- Ana Gomes (ed. lit.)
- Célia Gonçalves (ed. lit.)
- Lino André (ed. lit.)
- Nuno Bicho (ed. lit.)
- Tomasz Boski (ed. lit.)
Argitaletxea: Asociación Española para el Estudio del Cuaternario ; Grupo de Trabalho Português para o Estudo do Quaternário (GTPEQ)
Argitalpen urtea: 2017
Orrialdeak: 155-156
Mota: Liburuko kapitulua
Laburpena
This work characterizes the sedimentary facies of storms that are recorded in the upper reaches of the internal sand barriers at the mouth of the Roman paleo-estuary of Huelva (Palus Erebea). This storm facies reveals a very effective growth mechanism for the backshore área by means of its vertical aggradation and northward progradation during high-energy wave episodes. The calibrated and modelled radiocarbon dates in marine shells of Glycymeris provide a time range between the late 1st BC and the entire 2nd AD centuries.