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 200

Gamma Ray

Lithology/Core graph Interpretation

Strat.

0 API 200

Channel

Palaeosols (grey)

Fluvial
channel

Channel

Abandoned
channel

Fluvial
channel

Fluvial
channel

Coarse, fluvial
bedload

Fluvial
channel

Unconformity

Crevasse

Bay fill

Crevasse

Bay/lake

Palaeosols (mottled)

Lake (?)

Crevasse
splays

Lake / swamp

Clay Si vf f mcvccCgl

Grain size

Fig. 9. Cored section of the upper Fruholmen and Tubåen formations in well 7226/11-1, Norsel High. Note that the cored
section is plotted on a different vertical scale than the wire-line curve. For legend, see Fig. 5.