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 495

b8

ELGIN 22/30

FRANKLIN 29/5b

G7

C10

C8

Heather Fm

G5 F4

F1

G4

F2

6Z Franklin

C Sand

G8Y

c13

F3Z

Serratum mfs

SB

Unnamed mfs

Franklin
B Sand

Glosense mfs

ELGIN

2 km

100 m

Franklin
A Sand

N

FRANKLIN

Pentland Fm.

10 km

Fig. 17. Correlation of the Elgin and Franklin fields (from Wonham et al ., 2002). Comparison can be made with an earlier correlation of Lasocki et al . (1999)
which proposes a conformable succession. In this new correlation, the upper part of the Franklin B Sands can be seen to be significantly truncated in the
northern part of Elgin Field, removing the spicule-bearing sandstones in this area (yellow unit with green spots).