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Open to closed system transition traced through the TDIC isotopic signature at the aquifer recharge stage, implications for groundwater 14C dating
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Open to closed system transition traced through the TDIC isotopic signature at the aquifer recharge stage, implications for groundwater 14C dating
Gillon, M.
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Barbecot, F.
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Gibert, E.
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Corcho-Alvarado, J.A.
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Marlin, C.
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Massault, M.
- 2015
International audience
Accès au document
Lien externe vers le document:
https://hal.archives-ouvertes.fr/hal-00416553
Métadonnées du document
Auteur(s):
Gillon, M.
/
Barbecot, F.
/
Gibert, E.
/
Corcho-Alvarado, J.A.
/
Marlin, C.
/
Massault, M.
- 2015
Editeur:
HAL CCSD
Contributeur:
Interactions et dynamique des environnements de surface (IDES) ; INSU - Université Paris-Sud - Paris 11 (UP11) - CNRS
University Institute of Radiation Physics ; Université de Lausanne
Langue:
ANGLAIS
Candidats descripteurs:
[SDU.STU] Sciences of the Universe/Earth Sciences