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Geothermal state of the deep Western Alpine Molasse Basin, France-Switzerland

Auteur(s)
Chelle-Michou, C
Do Couto, D
Moscariello, A
Renard, Philippe 
Centre d'hydrogéologie et de géothermie 
Rusillon, E
Date de parution
2017
In
Geothermics, Elsevier, 2017/67//48-65
Mots-clés
  • Geothermal anomaly
  • Geostatistics
  • Structure
  • Alpine Molasse Basin
  • Fluid circulations
  • Bottom hole temperature
  • Geothermal anomaly

  • Geostatistics

  • Structure

  • Alpine Molasse Basin

  • Fluid circulations

  • Bottom hole temperatu...

Résumé
Over the last few years the Western Alpine Molasse Basin (WAMB) has been attracting large institutional, industrial and scientific interest to evaluate the feasibility of geothermal energy production. However, the thermal state of the basin, which is instrumental to the development of such geothermal projects, has remained to date poorly known. Here, we compile and correct temperature measurements (mostly bottom hole temperature) from 26 existing well data mostly acquired during former hydrocarbon exploration in the basin. These data suggest that the average geothermal gradient of the WAMB is around 25–30 °C/km. We further use these data to build the first well data-driven 3D geostatistical temperature model of the whole basin and generate probabilistic maps of isotherms at 70 and 140 °C. This model highlights a number of positive and negative thermal anomalies that are interpreted in the context of heat advection caused by fluid circulation along faults and/or karst systems. This study confirms that the WAMB has a great potential for low-enthalpy geothermal resources and presents a typology of advection-dominated potential targets.
Identifiants
https://libra.unine.ch/handle/123456789/3617
_
10.1016/j.geothermics.2017.01.004
Type de publication
journal article
Dossier(s) à télécharger
 main article: Chelle-Michou_C-Geothermal_state_of_the_deep-20180119.pdf (7.69 MB)
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