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Deep water circulation at the northern Pyrenean thrust: Implication of high temperature water-rock interaction process on the mineralization of major spring water in an overthrust area

M. Khaska 1 C. Le Gal La Salle 2 G. Videau J.-S. Flinois S. Frape P. Verdoux 2 M. Arnold 3 G. Aumaître 3 D.L. Bourles 3 K. Keddadouche 3
1 Laboratoire GIS
CEREGE - Centre européen de recherche et d'enseignement des géosciences de l'environnement
2 GIS - Laboratoire de Géochimie Isotopique Environnementale (GIS) / Université de Nîmes
3 CEREGE - Centre européen de recherche et d'enseignement des géosciences de l'environnement
Abstract : no abstract
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Journal articles
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https://hal-amu.archives-ouvertes.fr/hal-01458860
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Submitted on : Tuesday, February 7, 2017 - 9:34:40 AM
Last modification on : Wednesday, April 6, 2022 - 1:06:04 PM

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UNIV-AMU | CNRS | CEREGE | OSU-INSTITUT-PYTHEAS | CDF | INSU | UNIMES | INRA | INRAE | TP | PSL | LN2C

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M. Khaska, C. Le Gal La Salle, G. Videau, J.-S. Flinois, S. Frape, et al.. Deep water circulation at the northern Pyrenean thrust: Implication of high temperature water-rock interaction process on the mineralization of major spring water in an overthrust area. Chemical Geology, Elsevier, 2015, 419, pp.114-131. ⟨10.1016/j.chemgeo.2015.10.028⟩. ⟨hal-01458860⟩

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