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 515

Smørbukk

6506/11-2

6506/11-4

Smørbukk Fault

Trestakk-Smørbukk Fault

6406/2-3

Kristin

6406/2-5

(B)

NW SE WNW ESE

6406/2-3
Wells 6406/2-3T2

6406/3-2 6407/1-2 6407/6-5

0.0

Garn Fm.
Ile & Tofte
fms.
Tilje Fm.
Åre Fm.
(with marker
coal level)

1.0

Bremstein Fault

Cenozoic

2.0

Trestakk-Smørbukk Fault

Cretaceous

Melke & Spekk fms.

3.0

Klakk Fault

BCU

Garn-time Kristin
graben

Top of Triassic

4.0

5.0

~10 km

Sklinna
High

Kristin

Trestakk Tyrihans South Mikkel

6.0

Trøndelag
Platform

Halten Terrace

Fig. 2. (A) An eastward perspective view of the Halten Terrace structural image draped with a seismic-reflection intensity
map of 48-ms window below the base-Cretaceous reflector, sampling the Upper Jurassic. The zones of low intensity (blue-
green colours) are attributed to the erosion of the Upper to Middle Jurassic (Corfield & Sharp, 2000). (B) Geoseismic cross-
section through the Halten Terrace along the traverse line shown in Fig. 1 (left-hand map), with the BCU symbol denoting
the base-Cretaceous regional unconformity (modified from Martinius et al ., 2005).