The Glueckstadt Graben, a sedimentary record between the North and Baltic Sea in north Central Europe

The Glueckstadt Graben is one of the deepest post-Permian structures within the Central European Basin system and is located right at its “heart” at the transition from the North Sea to the Baltic Sea and from the Lower Saxony Basin to the Rynkoebing–Fyn High. The Mesozoic to recent evolution is inv...

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Veröffentlicht in:Tectonophysics 2005-03, Vol.397 (1), p.113-126
Hauptverfasser: Maystrenko, Yuriy, Bayer, Ulf, Scheck-Wenderoth, Magdalena
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Sprache:eng
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