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Inversion in the North Sea area and onshore Denmark is a well-known phenomenon and the main phase is interpreted to have occurred in the Cretaceous and early Cenozoic. This study demonstrates an important early Neogene inversion phase that resulted in the most distinct flexuring of the southern Danish Central Graben during the Cenozoic. Reactivation of structures on the Ringkøbing-Fyn High also took...
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