Eocene/Oligocene paleoceanography from ODP Hole 113-689B and Hole 113-690B
Middle Eocene to Late Oligocene sediments from near the crest (Site 689B, water depth 2080 m) and flank (water depth 2914 m) of the Maud Rise (62°S) have been investigated by coarse fraction analysis and have revealed the following: (1) The middle Eocene (50-40 Ma) was a period of pure carbonate sed...
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Format: | Dataset |
Language: | English |
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PANGAEA
1991
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.759819 https://doi.org/10.1594/PANGAEA.759819 |