Description
Deposits of the Middle Shell Lime are preserved only in the eastern part of the study area in edge sinks of salt structures. Further west, no mussel lime has been preserved due to the late Jurassic to Cretaceous erosion. The low altitude generally increases from north to south and reaches its maximum in the edges of the salt wall Linda/Liane. High altitudes are mainly located in the north of the study area.
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Tags
- geologie
- inspireidentifiziert