The Garn Formation (Bajocian-Bathonian) in the Kristin Field, Halten Terrace: its origin, facies architecture and primary heterogeneity model - From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin - page 513

6° 20 ʹ 6° 40 ʹ 7° 00 ʹ 7° 20 ʹ 7° 40 ʹ

65° 15 ʹ

Arctic Circle

N 66°30 ʹ

Vøring
Basin

Morvin

N 66°15 ʹ

N 66°00 ʹ

N 65° 45 ʹ

Yttergryta Halten

Terrace

Smørbukk

N 65° 30 ʹ

Tr øndelag
Platform

Smørbukk N 65° 1 5 ʹ

Lange South

N 65° 0 0 ʹ

Midgard

65° 00 ʹ

N 64° 45 ʹ

Sigrid

N 64° 3 0 ʹ

Erlend
North

Kristin

NORWAY

N 64° 15 ʹ

Ty rihans
North

E 12° 00 ʹ

E 11° 00 ʹ

E 6° 00 ʹ

E 9° 00 ʹ

E 10°00 ʹ

E 7° 00 ʹ E 8° 00 ʹ

Tr estakk

Erlend

N

N 63° 4 5 ʹ

0 20 km

N 63° 30 ʹ

Ragnfrid

Ty rihans
South
Main faults (tick on
downthrown side)

Tr ondheim

Lavrans

N

N 63° 15 ʹ

64° 45 ʹ

100 km

W E

N 6 3° 00 ʹ

Mikkel S

Fig. 1. The location of the Halten Terrace and adjacent structural units of the Norwegian Continental Shelf (right) and the location of the Kristin Field among
the terrace's petroleum fields (left). The blue line in the left-hand map indicates the cross-section shown in Fig. 2B and the blue frame indicates the study
area shown in Fig. 4.