The influence of shelf-crossing glaciation on continental slope sedimentation, Flemish Pass, eastern Canadian continental margin

Flemish Pass is a small, perched slope basin seaward of the Grand Banks on the eastern Canadian continental margin. Glacial ice crossed the Grand Banks to reach the upper continental slope during some Mid to Late Quaternary glaciations but terminated on the middle shelf, 200 km distant, at the last...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	Marine geology 2009-09, Vol.265 (1), p.67-85
Hauptverfasser:	Huppertz, Tammo J., Piper, David J.W.
Format:	Artikel
Sprache:	eng
Schlagworte:	eastern Canadian continental margin Flemish Pass Marine mass-transport deposits
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!