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