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Geothermal Energy

Science – Society – Technology

Fig. 7 | Geothermal Energy

Fig. 7

From: The Muschelkalk aquifer of the Molasse basin in SW-Germany: implications on the origin and development of highly saline lithium-rich brines in calcareous hydrothermal reservoirs

Fig. 7

Lithium versus chloride concentration in thermal waters of the Upper Muschelkalk and corresponding trendline (red line). Black dotted line corresponds to the trendline for deep thermal water in the URG (Drüppel et al. 2020). Seawater data (Li ~ 0.191 mg kg−1; Cl ~ 19,400 mg kg−1) from Riley and Tongudai (1964)

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