Halten Terrace Lower and Middle Jurassic inter-rift megasequence analysis: megasequence structure, sedimentary architecture and controlling parameters - From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin - page 217

5°E 6°E 7°E 8°E 9°E

A

A ʹ

B

B ʹ

50 km

High at Base Cretaceous
High at Base Tertiary
Inversion high

Late Triassic to Mid Jurassic fault
Late Jurassic fault
Late Cretaceous fault

(C)

NW Klakk

Fault
Complex

SE

Sklinna
Ridge

Kya Fault Zone
Grinda Graben

Gimsan
Basin

Bremstein
Fault Complex

Trøndelag
Platform

Rås Basin

(I)

Kristin Lavrans Tr estakk Ty rihans Mikkel Draugen

0 0

2
4
6
8
10

2
4
6
8
10
12
14

12
14

50 km

Halten Terrace

NW Klakk

Fault
Complex

SE

Sklinna
Ridge

Kya Fault
Zone

Vingleia Fault
Complex

Frøya Froan
High Basin

Rås Basin

(II)

Linnorm Njord

0
2
4
6
8
10
12
14

0
2
4
6
8
10
12
14

50 km

Halten Terrace

LEGEND

Neogene Cretaceous Triassic

Upper Palaeozoic

Basement

Palaeogene Jurassic

Fig. 2. Location map (A) and structural elements map (B) of the Halten Terrace area, mid Norway. (C) Regional geosection
across the Halten Terrace (modified from Osmundsen et al ., 2002).