Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5113604 | Quaternary International | 2017 | 9 Pages |
Abstract
The fossil travertine represents a 7Â ky-long record of CO2 leakage above a natural reservoir, from Late Pleistocene to Mid-Holocene. The flux of CO2 leakage through time and the total escaping volume have been computed and appears to be low in comparison with an anthropogenic leak provoked, for instance, by a non-sealed well.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Emanuelle Frery, Jean-Pierre Gratier, Nadine Ellouz-Zimmerman, Pierre Deschamps, Dominique Blamart, Bruno Hamelin, Rudy Swennen,