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 373

Å re 3 Tilje 1. 1. 1

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
Cross-bedding
Ripple cross-lamination
Bioturbated
Large Diplocraterion

Fluid mud deposits
Channel fills

FM

(C) (D)

Tilje 1. 1. 2

Tilje 1. 2

FM

FM

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
% Intense bioturbated
% Bioturbated sandstones
% Bioturbated reddish sands

FM

FM

FM

Lower-middle shoreface

Distributary mouth-bars
Laminated delta-front
Sediment dispersal pattern

Prox. Dist.

0 10 km

Coarse sand Medium sand Fine sand Very fine sand Mudstone

Fig. 20. Facies-distribution and palaeogeographic maps for the Smørbukk field from the upper Ǻre (A3) and lower-middle
Tilje (T1.1-T1.2). The maps integrate the structural background, sedimentary structures (processes) and dominant facies
associations (environments) for each reservoir zone. Active normal faults within the cover (after Marsh et al ., 2010) are