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Unité de recherche
INNOSUISSE
Numéro de projet
11950.1 PFIW-IW
Titre du projet
Introduction of micro-gravity as standard in geothermal exploration¿
Titre du projet anglais
Introduction of micro-gravity as standard in geothermal exploration¿

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 AllemandFrançaisItalienAnglais
Description succincte
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Résumé des résultats (Abstract)
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Textes saisis


CatégorieTexte
Description succincte
(Allemand)
Mikrogravimetrie als Standardprospektionsmethode für geothermische Reservoire
Description succincte
(Anglais)
Introduction of micro-gravity as standard in geothermal exploration¿
Résumé des résultats (Abstract)
(Allemand)
The productivity of a geothermal reservoir depends mainly on the transmissivity of the geological unit. It is a challenge to assess this during exploration. A first step is the assessment of porosity. Inversion of gravity based on 3D geology has revealed the thermal anomaly of Soultz-sous-Forêts. The aim is to further develop this methodology and to introduce it as a standard in the geothermal reservoir exploration in Switzerland.|The innovation is to put the focus on the evaluation of porosity changes in the target zones in combination|with detailed (3D) seismic studies, which reduce the uncertainty in the geological interpretation of gravity|data and thus allow the assessment of density changes due to porosity variation.
Résumé des résultats (Abstract)
(Anglais)
The productivity of a geothermal reservoir depends mainly on the transmissivity of the geological unit. It is a challenge to assess this during exploration. A first step is the assessment of porosity. Inversion of gravity based on 3D geology has revealed the thermal anomaly of Soultz-sous-Forêts. The aim is to further develop this methodology and to introduce it as a standard in the geothermal reservoir exploration in Switzerland.|The innovation is to put the focus on the evaluation of porosity changes in the target zones in combination|with detailed (3D) seismic studies, which reduce the uncertainty in the geological interpretation of gravity|data and thus allow the assessment of density changes due to porosity variation.