Fig. 3
Regional cross-section composed of facies logs of boreholes from northern Switzerland. Lithofacies association correlation is based on cyclostratigraphic correlations. Member divisions of the Upper Muschelkalk after Pietsch et al. (2016) are marked with dashed lines. The Stamberg Member is equivalent to the dolomitized sediments of the former Trigonodus Dolomit, while the combined 3 other members are equivalent to the former Hauptmuschelkalk. Note that the Bözberg borehole was drilled at a 45° angle relative to the Upper Muschelkalk bedding and thus appears longer than its true vertical thickness