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 315

TDSS

F Sf

D FTT

C

WDBE

FTT

FTT

FTT

TDSS

Locality S3

Section 4

(C)

(B)

Locality S3

Section 1

Key
surfaces

180

AU AE

Se ctio n 1 Section 4 Section 8

180

170

MTRS

170

170

FSf 160

fig.D

160

160

150

SU2/TS5

150

fig.C

150

140

TS4

140

(D) 140

130

Section 1

130

sand-
stone

130

120

120

MFS3

120

110

silt-
stone

110

110

100

mud-
stone

100

SU1/TS3

Sand

Sand Sand

Clay Silt Gr. Pbl. Clay Silt Gr. Pbl.

Clay Silt Gr. Pbl.

Fig. 10. (A) At locality S3 the architectural elements TDSS, FTT and WDBE are stacked in laterally identifiable successions
within the upper stratigraphical compartment (measured section 4, persons circled for scale). (B) Detailed sedimentary logs
through the AU4 to AU7 show sedimentology, architectural elements and key surfaces at locality S3. (C) Photo of abundant