Tectonic control on sedimentation, erosion and redeposition of Upper Jurassic sandstones, Central Graben, North Sea - From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin - page 475

WSW ESE

UK NO

Te rtiary
Cretaceous
Kimm. -Volg. Shales
Kimm. Shales
Oxfordian/Kimm Sst
Middle Jurassic
Tr iassic
Zechstein Salt
Rotliegendes

1000 m

10 km

Fig. 2. Regional structural section across the Central Graben showing some areas where salt is the dominant control on later structural development and
sedimentation (e.g. near the border region) and other areas where the salt is thinner and Upper Jurassic sedimentation is directly influenced by the move-
ment of Rotliegend faults (e.g. 2/4-20 well area). The geographical location of this geological section is indicated on Fig. 1.