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Abstract

Geothermal energy is an increasing part of the worldwide energy supply. There are three geological provinces in Germany with hydrogeothermal potential: the North German Basin, the Upper Rhine Graben, and the Southern German Molasse Basin. Within the Southern German Molasse Basin the hydrogeothermal aquifer comprises carbonate rocks of the Upper Jurassic which were lowered to a depth of approximately 3500 m.

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/content/papers/10.3997/2214-4609.201404962
2009-06-08
2024-04-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201404962
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