Abstract
Some years ago the thermal water wells of the spa Deutsch-Altenburg were considered the result of a local water circulation. Extensive measurements of the water chemistry, trace elements, and environmental isotopes combined with drillings in the river bed of the Danube resulted in the indication of a key position of the mineral thermal wells of Deutsch-Altenburg for the groundwater circulation in the entire Vienna basin. The proof of this fact demanded the inclusion of the complicated geological position of the basin into the argumentation.
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