Sedimentation at the Jurassic–Triassic boundary, south-west Barents Sea: indication of climate change - From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin - page 188

0°0 ʹ 10°0 ʹ 20°0 ʹ 30°0 ʹ

NKB

BB: Bjørnøya Basin
BP: Bjarmeland Platform
DT: Dønna Terrace
FP: Finnmark Platform
HFB: Hammerfest Basin
HT: Halten Terrace
LH: Loppa High
LM: Lofoten Margin
MB: Møre Basin
NKB: Nordkapp Basin
TB: Tromsø Basin
TP: Trøndelag Platform
SVB: Sørvestsnaget Basin
VB:

B P

BB

L H

F P

HF B

SVB

TB

70°0 ʹ

Vøring Basin

VG: Viking Graben

LM

V B

T P

65°0 ʹ

HT

MB

VG

60°0 ʹ

0 150 km

Faults Continent Ocean Boundary

Fig. 1. Main structural features and sedimentary basins of the Norwegian Continental Shelf (based on Gabrielsen et al .
1990; Blystad et al . 1995 and Færseth, 1996).