Pre-Wisconsin stratigraphy and paleoclimates off Atlantic Canada, and its bearing on glaciation in Québec

Cores from tops of seamounts close to the continental shelf west of the Grand Banks contain sequences of alternating clays (representing glacials) and foram nanno ooze (deposited in warmer periods), back to the Pliocene. Although sedimentation in the cores is controlled primarily by glacial conditio...

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Bibliographic Details
Published in:Géographie physique et Quaternaire
Main Authors: Alam, M., Piper, D. J. W.
Format: Text
Language:English
Published: Les Presses de l’Université de Montréal 1977
Subjects:
Online Access:http://id.erudit.org/iderudit/1000048ar
https://doi.org/10.7202/1000048ar