The long-term evolution of the Douro River as evidenced by strath terrace staircases located at NE Portugal (western Iberia)

In western Iberia, mechanisms that explain the transition from endorheic to exorheic continental-scale drainage reorganisation are foreland basin overspill, headwards erosion and capture by an Atlantic river, or a combination of both. To explore these controls we have investigated the Portuguese sec...

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Detalhes bibliográficos
Autor principal: Cunha, Pedro P. (author)
Outros Autores: Martins, António A. (author), Gomes, Alberto (author), Cabral, João (author), Lopes, Fernando C. (author), Pereira, D. I. (author), Vicente, Gerardo de (author), Buylaert, Jan-Pieter (author), Murray, Andrew S. (author), Stokes, Martin (author)
Formato: conferenceObject
Idioma:eng
Publicado em: 2019
Assuntos:
Ciências Naturais::Ciências da Terra e do Ambiente
Texto completo:http://hdl.handle.net/1822/72102
País:Portugal
Oai:oai:repositorium.sdum.uminho.pt:1822/72102

Texto Completo

http://hdl.handle.net/1822/72102

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