Unravelling the nature of deep-marine sandstones through the linkage of seismic geomorphologies to sedimentary facies; the Hermod Fan, Norwegian North Sea - From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin - page 650

Grid
Frigg
Hermod
Sediment
transport
directions
Oil and
gas fields

Oseberg
Field

Frigg Fan

NORWAY

Hermod Fan

SWEDEN

UK

DENMARK

Shetland Platform-
North Viking Graben

W E

Grid

II ʹ

Grid

I

Frigg

Frigg Field

Odin

Hermod (S2)

I ʹ
II

Hermod (S1)

Frøy Field

Heimdal
Heimdal

Alvheim
Field

Heimdal Field

Ty
Ty

0 15 km

Fig. 2. Lithostratigraphic columns and the plan-view distribution of a Hermod Fan, a Frigg Fan and a younger channel
complex assigned to the Grid Member. Line I-I' corresponds to well section of Fig. 15, line II-II' corresponds to well section
of Fig. 4.

(A) (B) (C)

26/4-2 26/4-2

ms twt

80
76
72
68
64
60
56
52
48
44
40

10Hz

13Hz 11Hz

The RGB Colour Chart

N

0 5km

Fig. 3. (a) Isochron map between reflectors near the top and base Sele Formation. (B) Time slice at 34 ms below the (near)