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 317

(A)

WDDL

TDDC

TDDF

TDDC

TDSS

FTT

Locality S5 WDBE

Section 13

Locality S5

(B)

(C)

Section 12 Section 13 Section 14 AE AU

SORT

240

TDDC

230

SU3/TS6

Section 14

220

(D)

TDSS

210

200

MFS5

FTT

200

190

SU2/TS5

fig.C

190

180

170

180

170

Section 14

160

170

160

Locality S5

(E)

150

Sections 13-14

160

150

140

MFS 5
FSf

150

140

MFS3

fig.D

130

SU2/TS5

140

130

120

130

TS4

120

TS4

SU1/TS3

110

MFS2

120

110

100

MFS3

110

100

13

90

Silt Sand

Silt Sand

Sand

Clay Gr. Pbl.

Clay Gr. Pbl.

Clay Silt Gr. Pbl.

14 sandstone siltstone mudstone

Fig. 12. (A) Photo of locality S5 (measured section 13) show the thick sandstone-dominated TDSS and FTT architectural ele-
ments indicating high rate of sediment input and rate of creation of accommodation space. The AU4 is interpreted as a major
distributary system (10 to 15 m thick and tens of metres-wide) at this locality. The overlying sandy heterolithic deltaic TDDC
and muddy heterolithic TDDF elements define the local deltaic system within an overall retrogradational AU5. Note that the
allostratigraphic unit AU6 is absent in this locality. (B) Detailed sedimentary logs show sedimentology, architectural elements
and key surfaces at locality S5 (measured sections 12 to 14). (C) Photo of a 12 m thick upward-coarsening deltaic architectural