Description
Deposits of the lower chalks are widespread in the study area and only have gaps along salt diapires in the eastern section. High altitudes are mainly formed above the salt cushions to the west and along the central salt wall, while the largest depths occur in the southern edge sinks around the central salt wall (Lollo/Lisa). Due to the erosion event at the base of the lower chalk, large parts of the Triassic sequences and the law in the case study region are not preserved.
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Tags
- geologie
- inspireidentifiziert