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Orientador(es)
Resumo(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.
Descrição
Palavras-chave
Sealevel rise Guadiana Estuary Postglacial Gulf of Cadiz
Contexto Educativo
Citação
Editora
Enrique Schnack & Colin Murray-Wallace
