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Inversion conjointe géophysique appliquée à l'exploration en géothermie profonde dans le Massif Central

Abstract : The development of geothermal energy has led to the exploitation of resources established in varied geological and geodynamic contexts. Geophysical exploration of these complex reservoirs requires the use of several complementary imaging methods. This PhD thesis focuses on the exploration of a geothermal resource located within the fractured basement in the French Massif Central using magnetotelluric, ambient noise tomography and gravimetry. Magnetotelluric is a 3D imaging method with a good resolution power that is sensitive to the presence of water and hydrothermal weathering clays but is limited by its spatial coverage. Seismic noise tomography has a good vertical resolution but does not resolve well horizontal velocity variations. This method is sensitive to variations of the mechanical properties of rocks and thus to fractured media. Finally gravimetry brings constraint on the lithological variations and has a good lateral resolution but lacks vertical resolution.We present a method of joint inversion of seismic and gravimetric data under the constraint of a resistivity model obtained by independent magnetotelluric inversion. Joint inversion requires defining model couplings. By lack of prior knowledge of petrophysical relationships, we have coupled the density, resistivity and velocity models with a law that constraints the parameters to be correlated on average.This strategy aims to bring out the characteristic relationships of the geological objects of the geothermal resource. This joint inversion methodology has been tested on synthetic models. The application to the real data acquired in the Massif Central has made it possible to define a deep zone of high correlation interpreted as the fragile ductile transition. The intermediate part of the models, more homogeneous, allows to distinguish different geological units separated by a fault zone. Finally the superficial part is distinguished by strong heterogeneity of the parameters resulting probably from surface alteration process.
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Submitted on : Friday, June 5, 2020 - 3:06:18 AM
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  • HAL Id : tel-02788190, version 1



Jean-Michel Ars. Inversion conjointe géophysique appliquée à l'exploration en géothermie profonde dans le Massif Central. Sciences de la Terre. Université de Bretagne occidentale - Brest, 2018. Français. ⟨NNT : 2018BRES0025⟩. ⟨tel-02788190⟩



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