The thickness of the Oligocene in the duck beak

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Provided by Bundesamt für Kartographie und Geodäsie

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Dataset information

Catalog

GDI-DE

Country of origin

Germany

Updated

2013.11.26 00:00

Created

2013.11.26

Available languages

German

Keywords

Geologie, inspireidentifiziert

Datasource

Official portal for European data link

Quality scoring

110

Dataset description

The maximum thickness between the base of the Oligocene and the base of the Burdigalium (near the base of the Lower Miocene) is approximately 700 m and is reached in a basin structure at the border with the Danish sector. In contrast to the width distribution of the layer pack of the lower Miocene, a shift of the depocenter to the central area of the duck beak can be seen. There is also an almost opposite sedimentation trend. The diapires in the area of the central trench appear clearly in the width distribution of this horizon.

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