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Within the frame of the ANR-funded CANTARE-Alsace project, we have undertakena multi-scale and multidisciplinary approach to increase our knowledge of thetransition zone between the sedimentary cover and the basement and providefundamental knowledge for the assessment of its geothermal potential. In thispaper, we report out the results of a study performed on an exhumed transitionzone in the Ringelbach area in the Vosges Mountains, on the flank of the Rhinegraben. In this analogue of a deeply buried transition zone of the RhineGraben, a thin layer of Triassic sandstones is still present on the top of thefractured and altered granitic basement providing the opportunity to studyin-situ the physical properties of this transition zone. In this paper, wefocused on electrical and acoustic properties of the transition zone as theyare the main physical parameters usually assessed with the help of geophysicalmethods during the exploration phase of a geothermal project.

Geophysical signature of the transition zone between the sedimentary  cover and the basement: an analogue approach to help de-risking geothermal  prospects