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 297

AU AE Locality S3 Key

surfaces

Sea-Level

section 1 section 4 section 8 section 10

fall

180

MFS5

180

MTRS

180

170

170

rise

FSf/
MTRS

170

170

160

160

SU2/TS5

E

160

160

150

150

fall

150

150

140

140

MFS4

140

140

rise

130

TS4

130

130

130

120

120

fall

120

120

MFS3

110

110

110

rise

110

100

100

SU1/TS3

overall rise in sea- level

100

100

90

Sand

Sand

Sand

Sand

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

Clay Silt Gr. Pbl.

Clay Gr. Pbl.

Silt

Sandstone Siltstone Mudstone

(B) (C) (D)

TDSS

WDBE

gneiss

Qz

T S4

WDBE

FTT

10cm

SU1/TS3, section 8, locality S3. SU2/TS5, section 28, locality N3. TS4, section 8, locality S3.

(E) (F)

1cm

FSf/MTRS, section 1, locality S3. FSf/MTRS, section 1, locality S3.

Fig. 5. (A) Selected detailed sedimentary logs (depths in m) through the upper stratigrahical compartment showing sedi-
mentology, key surfaces and changes in relative sea-level (locality S3). Photos of mixed regressive and transgressive lithofa-
cies overlying selected key surfaces at localities S3 and N3; (B) A matrix-supported conglomeratic bed overlying the SU1/