Uranium isotopes as tracers of groundwater evolution in the Complexe Terminal aquifer of southern Tunisia

The Complexe Terminal (CT) multi-layer aquifer is formed by Neogene/Paleogene sand deposits, Upper Senonian (Campanian-Maastrichtian limestones) and Turonian carbonates. The chemical composition and isotopes of carbon and uranium were investigated in groundwater sampled from the main hydrogeological...

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Veröffentlicht in:	Quaternary international 2020-05, Vol.547, p.33-49
Hauptverfasser:	Hadj Ammar, Friha, Deschamps, Pierre, Chkir, Najiba, Zouari, Kamel, Agoune, Aissa, Hamelin, Bruno
Format:	Artikel
Sprache:	eng
Schlagworte:	CT southern Tunisia Earth Sciences Holocene Mixing Radicarbon Sciences of the Universe Uranium isotopes Water-rock interaction
Online-Zugang:	Volltext
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