Applying accommodation versus sediment supply ratio concepts to stratigraphic analysis and zonation of a fluvial reservoir - From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin - page 112

Rockall High
(uplifted)

MB

(L.Sin.)

TS

FWSB

Fennoscandian
hinterland

SI VG

?

HP

(Hettangian)

SP

MFB

UH

(L.Sin.)

HE

Scotland

NDB

?

(Rhaetian)

(Hettangian)

DSB

CG

RFH

MNSH

(Rhaetian)

0 500 km

Continental Fluvial Marginal marine Shelf

Direction/timing of
marine inundation

Sediment transport direction

CG
DSB
FFZ
FWSB
HE
HP
MB
MFB

Central Graben NDB

MNSH
RFH
SI
SP
TS
UH
VG

Norwegian-Danish Basin

Danish Subbasin Mid North Sea High

Ringkøping-Fyn-High Fjerritslev Fault Zone

Faroe-West Shetland Basin Shetland Islands

Hebrides Basin Shetland Platform

Horda Platform Tempen Spur

Møre Basin Utsira High

Moray Firth Basin Viking Graben

Fig. 8. Schematic palaeogeographic map of the Statfjord Group (Raude and Eiriksson fms) in the Viking Graben (see Fig. 1)
and the area south of it during the Hettangian showing the inferred sediment transport patterns and general depositional
environments. Modified after Ryseth (2001) and Michelsen et al . (2003).