Influence of the Main Border Faults on the 3D Hydraulic Field of the Central Upper Rhine Graben

Figure 3

Cummulative thickness (a) of Cenozoic sediments, (b) of Keuper/Lias/Dogger, and (c) of Muschelkalk/Buntsandstein/Permo-Carboniferous (Pre-Keuper). The dashed line shows where the Keuper/Lias/Dogger sediments pinch out in reality. Maps are shown in UTM32N and rotated counter-clockwise by approximately 20°.