The interpretation of long term radon measure‐ments in a spring located in Vogtland shows a significant relationship to the seismicity of a region close to the sampling point. A statistical check was performed in order to identify the anomaly‐generating area. The cause for this relation is emission of mantle originated gases (including CO2) influenced by tectonic processes in the crust.
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Heinicke et al. (1995) studied this question.
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