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Publicação
Evolução geológica de Portugal continental durante o Cenozóico - sedimentação aluvial e marinha numa margem continental passiva (Ibéria ocidental)
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Orientador(es)
Resumo(s)
In Portugal mainland Cenozoic sedimentation occurred largely but allocated to several basins. Even in the same
basin, the sedimentary record shows significant lateral changes in facies and thickness. However, the main
sedimentary ruptures and overall lithologic characteristics of the infilling stages are quite similar in the several basins,
reflecting the geodinamic evolution of Iberia and the eustatic and climate changes during Cenozoic times. A
stratigraphic framework is proposed, in order to contribute towards a less complex use of the lithostratigraphic units
defined in the geological maps and literature. Some topics for future research are also suggested.
Descrição
6º Simposio sobre el Margen Ibérico Atlántico MIA09
Palavras-chave
Cenozóico Litostratigrafia Bacias sedimentares Portugal Cenozoic Lithostratigraphy Sedimentary basins
Contexto Educativo
Citação
Editora
Departamento de Geología, Universidad de Oviedo