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 332

0 ° 2 ° 4 ° 6 ° 8 ° 10 ° 12 °

68 °

67 °

V e stfjord
Basin

Træna
Basin

H e lgeland
Basin

66 °

Jameson
Land
Basin

Trøndelag
basin

65 °

Halten
basin s

Grip
land

64 °

Froan
Basin

Vigra
land

63 °

Kristiansund

Molde ~100 km

Areas subjected to erosion

Alluvial plain - mud and sand

Tsikalas et al. (2005; 2008) magnetic and/or
gravity anomalies indicating palaeo-highs

Shallow marine - sand

62 °

Mari n e-mud,
dark blue=deeper water

Hamann et al. (2005, fig. 3) stipulated NE-
Greeland highs below basalt.

Fig. 16. Early Jurassic palaeo-reconstruction of the Norwegian-Greenland Sea (modified from original figure by J. Gjelberg
in Johannessen & Nøttvedt, 2008; palaeo-highs from Tsikalas et al ., 2005, 2008; Hamann et al ., 2005; Berger & Jokat, 2008).
Drainage areas and suggested main depositional systems, as well as present day main faults and wells on the Norwegian
offshore, are indicated. Terminology modified from Blystad et al . (1995).