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Late Eocene- Oligocene magnetostratigraphy and biostratigraphy at South Atlantic DSDP site 522.

Geology
By: , and 

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Abstract

Upper Eocene to lowest Miocene sediments recovered at DSDP Site 522 in the S Atlantic Ocean allow direct calibration of magnetostratigraphy and calcareous plankton biostratigraphy. The results from Site 522 show that the Eocene/Oligocene boundary occurs in the reversed interval of magnetic Chron C13 (= C13R) and that the Oligocene/Miocene boundary probably occurs in the upper part of Chron C6C.-Authors
Publication type Article
Publication Subtype Journal Article
Title Late Eocene- Oligocene magnetostratigraphy and biostratigraphy at South Atlantic DSDP site 522.
Series title Geology
Volume 10
Issue 10
Year Published 1982
Language English
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Geology
First page 508
Last page 511
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