Evidence for an earliest Oligocene ice sheet on the Antarctic Peninsula
There is growing consensus that development of a semipermanent ice sheet on Antarctica began at or near the Eocene-Oligocene (E-O) boundary. Beyond ice-rafted debris in oceanic settings, however, direct evidence for a substantial ice sheet at this time has been limited and thus far restricted to Eas...
Published in: | Geology |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2006
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Subjects: | |
Online Access: | http://www.vliz.be/nl/open-marien-archief?module=ref&refid=231700 |