Transição do enchimento terciário para o encaixe fluvial quaternário na área de Vila Velha de Ródão (sector NE da Bacia do Baixo Tejo)

The geomorphologic characteristics and lithostratigraphic units of the transition from the Tertiary filling stage to the Quaternary fluvial incision in the Vila Velha de Ródão area (Lower Tagus Basin, NE sector) are presented. Several morphodynamic episodes, which had an important tectonic control,...

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Detalhes bibliográficos
Autor principal: Cunha, Pedro Proença (author)
Outros Autores: Martins, A. A. (author)
Formato: article
Idioma:por
Publicado em: 2010
Assuntos:
Geomorphology
lithostratigraphy
terraces
neotectonics
Quaternary
Lower Tagus Basin
Central Portugal
Texto completo:http://hdl.handle.net/10362/4706
País:Portugal
Oai:oai:run.unl.pt:10362/4706
Descrição
Resumo:The geomorphologic characteristics and lithostratigraphic units of the transition from the Tertiary filling stage to the Quaternary fluvial incision in the Vila Velha de Ródão area (Lower Tagus Basin, NE sector) are presented. Several morphodynamic episodes, which had an important tectonic control, were distinguished. The same main morphosedimentary processes can be identified in other areas of this important river basin. Five periods of Quaternary fluvial incision were characterized.

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