1887

Abstract

The Roar structure is situated in the Danish Central Graben and is surrounded by the Bo, Boje, Adda, Tyra and Jens structures. It is a low relief porous chalk closure generated by structural inversion during the Late Cretaceous and Tertiary periods. In addition, the general increase in subsidense toward the center of the Central Graben in Tertiary times has also influenced the structural evolution.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201410892
1991-05-28
2020-08-08
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410892
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error