Depositional dynamics and sequence development in a tidally influenced marginal marine basin: Early Jurassic Neill Klinter Group, Jameson Land Basin, East Greenland - From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin - page 316

Locality S4

Section 10

AU AE

Locality S4

200

TDEC

190

WDDL

Palaeogene sill intrusives

MFS5

180

WDDL

FSf

FTT

170

WDBE

160

150

MFS4

140

Locality S4

130

120

110

100

90

sandstone siltstone mudstone dolerite sill intrusives

Clay Sand

Silt Gr. Pbl.

Fig. 11. (A) A detailed sedimentary log through AU3 to AU7 showing sedimentology, architectural elements and key sur-
faces within the upper stratigraphical compartment at locality S4 (measured section 10). The compartment is here sand-
stone-dominated and composed of upward-coarsening and -fining units. (B) Photo of the locality S4. In the uppermost part
of the compartment, the sandstone-dominated WDDL architectural element is split by an irregular 10 to 15 m thick
Palaeogene dolerite sill intrusion. Photographs of lithofacies above the SU2/TS5 unconformity contain; (C) mixed belem-
nites and gravel; and (D) rare silicified tree trunks. (E) At locality S4, the lower part of the upper stratigraphical compart-