Advisor(s)
Abstract(s)
In the Guadiana River Estuary, the Holocene estuarine infill is underlain by coarse delta fan sediments enclosing saltmarh deposits, dating back to isotope stage 5e or a stage 3 interstadial highstands.
Description
Keywords
Sealevel rise Guadiana Estuary Postglacial Gulf of Cadiz
Citation
Publisher
Enrique Schnack & Colin Murray-Wallace