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 320

(A)
AU

Locality N1 Locality N2 Locality N3 Locality N4

(B)

Localities N1-3, measured sections 18-29

AE

Section 18 Section 19 Section 23 Sections 27 & 28 Section 29

MFS5

FSg

SU3/TS6

260 40

SU3/TS6

30

230 250

20

220 240

M FS5

FS-f

210 10

230

SU2/TS5

SU1/TS3

0m

200 220 sub-aerial

sub-aquaous

240

MFS5

Silt Sand

Clay Gr. Pbl. 40 NNW ~16-km SSE

heterolithic

70

190 210

230

sandy

30

60

200

180 220

20

50

170 190

210

Fig.C

10

FSf

40

160 180

200

0m

30

150 170

Silt Sand

190

Clay Gr. Pbl.

20

140 160

180

10

130 150

170

Fig.D

SU2/TS5 0m

140

120

160

Silt Sand Clay

Gr. Pbl.

MFS3

110 130

150

100 120

Qz

140

Qz

90 110

SU1/TS3

130

80 100

120

Silt Sand Clay

Silt Sand Clay

Gr. Pbl.

Gr. Pbl.

110

Silt Sand sandstone siltstone mudstone

Clay

Gr. Pbl.

(E)

Locality N2

Section 23

Fig. 13. (A) Detailed sedimentary logs (depths in m) showing sedimentology, architectural element and key surfaces in the
northern area (localities N1 to 4). (B) A schematic presentation of a possible depositional scenario for the AU8. Note the rela-
tively similar palaeocurrent directions. (C) Photo of upward facies transition across the flooding surface FSf that separates the
sandy heterolithic TDEC and muddy heterolithic WDDL elements at locality N4 (measured section 29). (D) Photo of matrix-
supported conglomerate bed directly overlying the combined SU2/TS5 unconformity surface at locality N3 (measured sec-