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...
Published in: | Sedimentology |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
1992
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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 |