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 206

7121/5-1

7226/11-1 RHOB

7124/3-1

NPHI

RHOB

RHOB

NPHI

NPHI

?

Tidal deposits Coal layer/roots

Delta/coastal plain (heterolithic/coal bearing) Biostratigraphic timeline

Fluvial channels, (sand-dominated) RHOB Bulk density

Neutron porosity

Offshore/pro-delta NPHI

Shoreface/delta mouth-bar

Fig. 12. Correlation of Late Triassic to Early Jurassic strata in the south-west Barents Sea. The upper part of the Snadd Formation
and upper part of the Fruholmen Formation are characterised by channelised sandstone units encased within the surrounding
floodplain/delta plain deposits. The overlying Tubåen Formation forms a multilateral/multi-storey sandstone body of nested
fluvial channel sandstones. For well locations, see Fig. 2B.