Evolution of Fluid Circulation in the Rhine Graben: Constraints from the Chemistry of Present Fluids

Author:

Aquilina L.,Genter A.,Elsass P.,Pribnow D.

Publisher

Springer Netherlands

Reference68 articles.

1. Aquilina, L., Sureau, J.F., Steinberg, M. and the GPF team (1997a) Comparison of surface-, aquifer-, and pore waters from a Mesozoic sedimentary basin and its underlying Paleozoic basement, southeastern France: chemical evolution of waters with diagenesis and relationship between aquifers, Chemical Geology 138, 185–209.

2. Aquilina, L., Pauwels, H. and Fouillac, C. (1997b) Water-rock interaction processes in the Triassic sandstone and the granitic basement of the Rhine Graben: geochemical investigation of a geothermal reservoir, Geochim. et Cosmochim. Acta 61, 4281–4295.

3. Aquilina, L. (1997c) Les circulations de fluides actuelles dans la croûte continentale supérieure (0.5–15 km). BRGM Report R39497, 66 p.

4. Aquilina, L. and Brach, M. (1995) Characterization of Soultz hydrochemical system: WELCOM (Well Chemical On-line Monitoring) applied to deepening of GPK-1 borehole, Geotherm. Sci. and Tech. 4, 239–251.

5. Ayt Ougougdal, M., Cathelineau, M., Pironon, J., Boiron, M.C., Banks, D. and Yardley, B. (1995) Diagenetic salt-rich and organic-rich fluid migration in the Rhine Graben Triassic sandstones (Soultz deep drilling), European Union of Geosciences, April 9–13 Strasbourg, Terra Abstracts 7, 198.

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