Groundwater evolution in the Continental Intercalaire aquifer of southern Algeria and Tunisia: trace element and isotopic indicators-Reference-Cited by-同舟云学术

Groundwater evolution in the Continental Intercalaire aquifer of southern Algeria and Tunisia: trace element and isotopic indicators

Published:2003-06 Issue:6 Volume:18 Page:805-822
ISSN:0883-2927
Container-title:Applied Geochemistry
language:en
Short-container-title:Applied Geochemistry

Author:

Edmunds W.M,Guendouz A.H,Mamou A,Moulla A,Shand P,Zouari K

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Pollution,Environmental Chemistry

Reference26 articles.

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3. Bath, A.H., Edmunds, W.M., Andrews, J.N., 1979. Palaeoclimatic trends deduced from the hydrochemistry of a Triassic sandstone aquifer. In: Proc. Internat. Symp. Isotope Hydrology, Vol. III, Vienna, pp. 545–568.

4. Geology of Tunisia and adjacent parts of Algeria and Libya;Bishop;Bull. Am. Assoc. Petrol. Geol.,1975

5. Bassin sédimentaire du Sahara septentrional (Algérie-Tunisie). Aquifères du Continental Intercalaire et du Complexe terminal;Castany;Bull. BRGM 2,1982

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