The Ormen Lange turbidite systems: sedimentary architectures and sequence structure of sandy slope fans in a sediment-starved basin - From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin - page 611

6305/1- 1 6305/4-1 6305/8-1

6305/5-16305/7- 1 6305/9-1 6305/12-1,2 6305/3-1 6306/10-1 6306/6-1

Tectonic history
CMB

MFS

MMH/WMB MM

Ta re

Tang

Egga

Springar

Nise

Kvitnos

Lysing

6305/4-1 305/8-1
6305/5-1

(B)

6305/1- 1 6305/7- 1 305/9-1 6305/12-1,2 6305/3-1 6306/10-1 6306/6-1

Tectonic history
CMB MMH/WMB MM

55
56
57
58
59
60
61
62
63
64
65
66
67
68
69
70
71
72
73
74
75
76
77

Ta re

R

Tang

R

Egga

R

Springar

R?

Deepseated faulting with
sediment folding/flexuring
Uplift

MMH/WMBMøre Marginal High/
Western Møre Basin

Sand-prone
Shallow to deep marine

Tilting

Shelf
Slope
Basin floor

CMB
MM

Central Møre Basin
Møre Margin

Extensional
faulting

Sliding/Slumping

Fig. 2. (A) Upper Cretaceous and Lower Palaeogene tectono-stratigraphy of the Møre Basin. (B) Detailed Maastrichtian to
Palaeocene tectono-stratigraphy of the Møre Margin and eastern Møre Basin.