Glacial oscillations during the Bølling–Allerød Interstadial–Younger Dryas transition in the Ruda Valley, Central Pyrenees

The Upper Garonne Basin included the largest glacial system in the Pyrenees during the last glacialcycle. Within the long‐term glacial retreat during Termination‐1(T‐1), glacier fluctuations left geomorphic evidencein the area. However, the chronology of T‐1 glacial oscillations on the northern slop...

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Detalhes bibliográficos
Autor principal: Fernandes, Marcelo (author)
Outros Autores: Oliva, Marc (author), Vieira, Gonçalo (author), Palacios, D. (author), Fernández-Fernández, Jose M. (author), Garcia‐oteyza, J. (author), Schimmelpfennig, I. (author), Team, Aster (author), Antoniades, D. (author)
Formato: article
Idioma:eng
Publicado em: 2022
Assuntos:
Bølling–Allerød
Central Pyrenees
Cosmic‐ray exposure dating
Deglaciation
Younger Dryas
Texto completo:http://hdl.handle.net/10451/51552
País:Portugal
Oai:oai:repositorio.ul.pt:10451/51552

Texto Completo

http://hdl.handle.net/10451/51552

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