| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9461890 | Comptes Rendus Geoscience | 2005 | 8 Pages |
Abstract
We calculate the chemical depletion fraction of the granitic bedrock by analysing the rock-soil enrichment of zirconium. In Vendée (France), chemical weathering rates account for 26% of the denudation rates. Such a chemical depletion fraction characterizes temperate regimes. It is three times lower than that of humid tropical regimes. To cite this article: J.-C. Maurin et al., C. R. Geoscience 337 (2005).
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
Jean-Christophe Maurin, Françoise Gilbert, Michel Robert, Carine Churlaud,