Plio‐Pleistocene sedimentation in Ferrar Fiord, Antarctica

ABSTRACT A 166 m thick Plio‐Pleistocene sequence of glacial sediments has been cored in Ferrar Fiord in the southwestern corner of the Ross Sea, Antarctica. The core has the following lithofacies: massive diamictite (33% of the core; interpreted as lodgement or waterlain till), weakly stratified dia...

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Bibliographic Details
Published in:Sedimentology
Main Authors: BARRETT, P. J., HAMBREY, M. J.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1992
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1365-3091.1992.tb01025.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-3091.1992.tb01025.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-3091.1992.tb01025.x