| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4719868 | Marine Geology | 2006 | 10 Pages |
Abstract
The differences observed between present-day samples from Congo channel and from the terminal depositional lobe suggest a segregation of the sand along the channel during the transit which creates a Pb isotopic fractionation. Therefore, the comparison between Sr and Pb isotopes shows a strong discrimination of Pb according to sedimentation processes while Sr isotopes seem directly influenced by the coastal rivers contributions.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Yasmine Bentahila, Olivier Hebrard, Dalila Ben Othman, Jean-Marc Luck, Michel Seranne, Michel Lopez,