Practical use of advance software in an interactive stratigraphic and structural analysis of roar field: A case history

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.