| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6334966 | Applied Geochemistry | 2015 | 14 Pages |
Abstract
The maximum estimated uncertainty due to variations in the δ18O value over time is 202 m. Use of H isotopes is not recommended for constraining average recharge elevations due to important local variations, reflecting in different relations for the Coastal Chain and the Sila Massif. Assuming that Equation (1) holds true throughout Northern Calabria, an iso-distribution map of the δ18O value in rainfall has been drawn for this area.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Giovanni Vespasiano, Carmine Apollaro, Rosanna De Rosa, Francesco Muto, Salvatore Larosa, Jens Fiebig, Andreas Mulch, Luigi Marini,