Fig. 3From: 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 reservoirsTemperature distribution in the Upper Muschelkalk aquifer (after Stober and Jodocy 2009a, 2009b), showing significantly elevated temperatures along a SE–NW oriented ‘line’ (W of Bad Waldsee–Saulgau to E of Sigmaringen)Back to article page