Clay-mineral signatures of fossil and active hydrothermal circulations in the geothermal system of the Lamentin Plain, Martinique
Résumé
Whereas the study of clay minerals (using parameters such as structure modifications, crystal chemistry) has proved to be an effective approach in order to mark the circulation zones and fluid temperatures in high-temperature systems, there is an important lack of data dealing with such problems in moderate- to low-temperature systems. This paper proposes to fill this lack by studying the site of the Lamentin Plain (Martinique), characterized by a low-temperature geothermal activity (50°C
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Sciences de la TerreFrédérique COUFFIGNAL : Connectez-vous pour contacter le contributeur
https://brgm.hal.science/hal-04083539
Soumis le : jeudi 27 avril 2023-14:05:25
Dernière modification le : mercredi 31 janvier 2024-17:30:08
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Identifiants
- HAL Id : hal-04083539 , version 1
- DOI : 10.1016/S0377-0273(03)00044-1
Citer
A Mas, P Patrier, D Beaufort, Albert Genter. Clay-mineral signatures of fossil and active hydrothermal circulations in the geothermal system of the Lamentin Plain, Martinique. Journal of Volcanology and Geothermal Research, 2003, 124 (3-4), pp.195-218. ⟨10.1016/S0377-0273(03)00044-1⟩. ⟨hal-04083539⟩
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