The maximum thickness of the Keuper between the base of the Keuper and the base of the Lower Jura, as well as the Jurassic and Cretan discordances in the top of the unit, is approximately 1 800 m and is reached in the southwest along the North Shillgrund disturbance. Also increased widths can be found in lowered areas such as the Mads trench, which allowed the preservation of sediments of the keuper before subsequent erosion.
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