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 sedi...

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Bibliographic Details
Main Author: Diester-Haass, Lieselotte
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1991
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.759819
https://doi.pangaea.de/10.1594/PANGAEA.759819