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 330

T-R 6

T-R 5

SU3/TS6
SU2/TS5

MFS5

TS6

SU1/TS3 SU3

N4 N3 N2 N1

TS5

rise

MFS1

fall

SU2

rise

TS1

S6

S5

S4

S3

Rævekløft Fm.
(WIBE)

Rævekløft Fm. (SHFS)

ESE

NNE

(B) T-R 5

T-R 5

T-R 4

SU2/TS5

MFS5

SU1/TS3

N4 N3 N2 N1

MFS1

MFS4

TS5

TS1

fall

S6

SU2

rise

fall

S5

S4

S3

Rævekløft Fm.
(WIBE)

Rævekløft Fm. (SHFS)

ESE

NNE

(A)

T-R 2

T-R 3

T-R 2

SU1/TS3

T-R 1

MFS3

N4 N3 N2 N1

MFS2

MFS1
TS1

TS3

TS2 SU1

S6

rise

fall

rise

S5

S4

S3

Rævekløft Fm.
(WIBE)

Rævekløft Fm. (SHFS)

Hinterland
Delta Plain
Sandstone (SHFS/TDDF/TDDP)

ESE

Wave/tide-dominated shale (TDDF/WDBE)

Brackish Shale (WIBE)

NNE

Alluvial Plain/Lacustrine shale

Crystalline Basement

Fig. 15. Successive stages in the development of depositional environments in the eastern Jameson Land Basin. The three
block-diagrams correspond to the stratigraphic intervals and systems tracts (Figs 7 and 14). The three sketches illustrate a