4 documents found, page 1 of 1
Geomorphic markers of Quaternary tectonics in Westernmost Iberia: insights from...
Martins, António; Cunha, Pedro; Gouveia, Margarida; Gomes, António Alberto; Falguères, Christophe; Stokes, Martin; Voinchet, Pierre; Cabral, João
The long-term evolution of the Douro River as evidenced by strath terrace stair...
Cunha, Pedro P.; Martins, António A.; Gomes, Alberto; Cabral, João; Lopes, Fernando C.; Pereira, D. I.; Vicente, Gerardo de; Buylaert, Jan-PieterIn 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 sector of the Douro River, the site of drainage re-organsation. The Douro River routes downstream through weak sedime...
Mechanisms and age estimates of continental-scale endorheic to exorheic drainag...
Cunha, Pedro P.; Martins, António A.; Gomes, Alberto; Stokes, Martin; Cabral, João; Lopes, Fernando C.; Pereira, D. I.; Vicente, Gerardo deIn western Iberia, mechanisms that can explain the transition from endorheic to exorheic continental-scale drainage reorganization are foreland basin overspill, headwards erosion and capture by an Atlantic river, or a combination of both. To explore these, we have investigated the Portuguese sector of the Douro River, the locus of drainage reorganization. The Douro River is routed downstream through the weak se...
The long-term evolution of the Douro River as evidenced by strath terrace stair...
Cunha, Pedro P.; Martins, António A.; Gomes, António Alberto; Cabral, João; Lopes, Fernando C.; Pereira, Diamantino; Vicente, Gerardo de