| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 7453269 | Quaternary International | 2010 | 13 Pages |
Abstract
The magnetic polarity of the WRFB sediments is normal. The palaeomagnetic data indicates that the sediments are of Brunhes Chron age, and imply that they post-date mid-MIS 19.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
P.L. Gibbard, S. Boreham, J.E. Andrews, B.A. Maher,