Eustatic, tectonic and climatic controls on an early syn-rift mixed-energy delta, Tilje Formation (Early Jurassic, Smørbukk field, offshore mid-Norway) - From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin - page 376

(A) (B)

Tilje 2

Tilje 3.1

FM

FM

FM

FM

Legend Part I
Post Tilje Fm fault
Active fault during Tilje Fm
deposition
Cored well
HCS
Wave ripple
Combined flow ripples
Low angle cross bedding
Wavy lamination

FM

FM FM

FM

FM

FM

FM

Horizontal lamination

Cross-bedding
Ripple cross-lamination

FM

FM

Bioturbated
Large Diplocraterion

FM Fluid mud deposits

Channel lags/gravel
Channel fills

(C) (D)

Tilje 3.2 T1lje 4

FM

FM

FM

FM

Legend Part II
% HCS
% Cross-bedded sandstone
% Clean ripple cross-laminated sands
% Sand dominated heterolithics
% Mixed sand-mud heterolithics
% Mud dominated heterolithics

FM

FM

FM

FM

FM

FM

FM

FM

FM FM

FM

% Pin-striped laminated mudstones

% Bioturbated heterolithics

% Bioturbated sandstones

FM

FM

% Bioturbated reddish sands

Tidal-Fluvial Channels

Heterolithic mouth bars

Interdistributary bays

Laminated delta front

Storm influenced delta front

Sediment dispersal pattern

0 10 km

Coarse sand Medium sand Fine sand Very fine sand Mudstone

Fig. 21. Facies-distribution and palaeogeographic maps for the Smørbukk field from the lower-middle (T2 to T3.1) and
middle-upper (T3.2 to T4) Tilje. See caption of Fig. 20 for explanation of symbols.