Glacial advance and retreat sequences in a Permo‐Carboniferous section, central Transantarctic Mountains
ABSTRACT Episodes of glacial advance and retreat can be recognized through analysis of vertical facies sequences in the Permo‐Carboniferous Pagoda Formation of the Beardmore Glacier area, Antarctica. The formation includes a remarkably complete record of continental sedimentation near the terminus o...
Published in: | Sedimentology |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Wiley
1989
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Online Access: | http://dx.doi.org/10.1111/j.1365-3091.1989.tb00617.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-3091.1989.tb00617.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-3091.1989.tb00617.x |