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Fig. 1 | Geothermal Energy

Fig. 1

From: Ground motions induced by pore pressure changes at the Szentes geothermal area, SE Hungary

Fig. 1

a Depth of the pre-Cenozoic basement showing the most significant sub-basins and hills of Hungary, and the location of the Szentes Geothermal Field, based on Haas et al. (2014) and modified after Békési et al. (2018). b Interpreted composite reflection seismic transect from the eastern part of Hungary, with the main tectonic and stratigraphic features of the area, after Balázs et al. (2016)

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