Depositional dynamics and sequence development in a tidally influenced marginal marine basin: Early Jurassic Neill Klinter Group, Jameson Land Basin, East Greenland - From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin - page 296

72°

25° 24° 23° 22°

71 ′ 5°

Gule Horn

N4

N3

Liaselv

Lepidop-

N2

teriselv

N1

Pase-Elv

Jameson
Land

71°

Hall B redning

S8
S7

Dusen Bjerg

Elis Bjerg

Liverpool
Land

Nathorst Fjeld

S6

Te rtiary volcanics

Constable Point
Airfield

Harris Fjeld

S5

Cretaceous

Hare-Elv

Jurassic Moskusoksekløft

S4

Astartekløft

Neill Klinter Group

S3

Skævdal/Albuen

Tr iassic

70 ′ 5°

S2

Permian

S1

Carboniferous

Devonian

Crystalline basement

24° 23° 22°

Fig. 4. Geological map of the Jameson Land region showing the outcrop of the Neill Klinter Group (in orange). The inves-
tigated localities in this study are S3 to 6 in the southern area and N1 to 4 in the northern area. Sections in localities S1 to
2 and S7 to 8 area are redrawn from Dam & Surlyk, 1998.