Sedimentation at the Jurassic–Triassic boundary, south-west Barents Sea: indication of climate change - From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin - page 199

Strat.

0 API 200

Lithology/Core graph Interpretation

Unconformity

Braided fluvial
system

lnterdistributary
bay-fill
Crevasses

Coal

Swamp/lake
Distributary channel

Coal

lnterdistributary
bay/lagoon

Major distributary
channel complex

Mouth bar

Pro-delta
mudrocks

Trangressive,
shallow marine
sandstone

Ravinement

Distributary channel

Lower delta
plain

Grain size

Fig. 8. Cored section and Gamma Ray curve from Early Norian to Rhaetian strata (Snadd, Fruholmen and lowermost
Tubåen formations) in well 7124/3-1, located in the transition zone between the Hammerfest Basin and the Nordkapp
Basin. For legend, see Fig. 5.