Location of known and suspected tectonic disturbances based on the Geological Map 1:200,000 (Guek 200). Along the disturbances, the rocks experienced a strong strain, can be shifted against each other and have lost their natural stability and hardness. The construction and operation of geothermal probes in the field of disturbances can lead to serious damage. Due to different topographical map bases, deviating representations to the tectonic disturbances of the geological map 1:500,000, 1:100,000 and 1:25,000 may occur.
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