Fig. 5From: 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 reservoirsTDS (a) and Cl (b) concentrations versus depth (data: Stober 2014). The TDS and Cl increase with depth is reaching a limit in about 1300–1500 m depthBack to article page