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Hydrogeothermal conditions in the Busko area within Cenomanian, Jurassic and Devonian aquifers are evaluated. Particularly favourable geothermal conditions in this area result from good hydrogeological parameters of the Cenomanian sandstone and limestone at the bottom of Jurassic deposits. Currently, other aquifers in this area: Devonian, Carboniferous and Triassic are regarded as being of secondary...
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