Depositional Environments and History of Late Quaternary Sediments in Hudson Strait and Ungava Bay: Further Evidence from Seismic and Biostratigraphic Data

Regional ship-borne investigations of seafloor sediments provide further information on late Quaternary depositional environments and history in the Hudson Strait-Ungava Bay region. Greatest sediment thicknesses, up to 130 m, occur in the large basin in eastern Hudson Strait and in the western Hudso...

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Bibliographic Details
Published in:Géographie physique et Quaternaire
Main Authors: MacLean, Brian, Vilks, Gustav, Deonarine, Bhan
Format: Text
Language:English
Published: Les Presses de l'Université de Montréal 1992
Subjects:
Online Access:http://id.erudit.org/iderudit/032917ar
https://doi.org/10.7202/032917ar