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 202

Strat. Lithology/Core graph Interpretation

0 API 200

Sub-tidal flats

Tr ansgression

Distributary
channel

Major
mouth bar

Wave-dominated
embayment

Tr ansgression

Multistorey /
multilateral
channel complex

Abandoned channel

Fluvial channel

Minor channel

Lagoon/bay

Crevasse channel

Coal
Coal

Delta plain

VF FM

SAND

C C

CLAY ILT CGL

Grain size