Middle Miocene Grounding Events on the Ross Sea Outer Continental Shelf, Antarctica
The middle Miocene δ<sup>18</sup>O enrichments from deep-sea data and eustatic sea level falls are traditionally attributed to expansion of the East Antarctic Ice Sheet. Interpretations of such data have led many to conclude that the West Antarctic Ice Sheet (WAIS) was not well-developed...
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| Format: | Others |
| Language: | en |
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LSU
2003
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| Online Access: | http://etd.lsu.edu/docs/available/etd-0822103-121632/ |