| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4704860 | Geochimica et Cosmochimica Acta | 2007 | 8 Pages |
Abstract
The good agreement between this experimental study and the two previous investigations demonstrates that Pb diffusion was measured in each case. It confirms that most of the perturbations in U-Th-Pb ages of monazite cannot be attributed to Pb diffusion.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Emmanuel Gardés, Jean-Marc Montel, Anne-Magali Seydoux-Guillaume, Richard Wirth,