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 309

NEILL KLINTER GROUP - JAMESON LAND, EAST GREENLAND

South ~105 km along depositional strike North

S1 S2 S3 S4 S5 S6 S7 S8 N1 N2 N3 N4

No outcrops
~35km

a b 1 8 10 12 15 16 c d 18 19 23 27/28 29/30

SORT
TDEC

SORT

AU8

TDEC

TDDF TDEC

TDEC

WDDL
TDSS

WDDL

AU7

WDDL

TDSS

FTT WDDL

AU6

TDEC

FTT

TDDC

WDBE

WDBE

AU5

TDEC

FTT

FTT

TDSS

TDSS

AU4

TDSS

FTT

FTT

WDBE

AU3

TDSS

AU2

TDDP

TDDP

TDDF

AU1

SHFS

KSG

ARCHITECTURAL ELEMENTS

The Kap Stewart Group (Alluvial plain - lake complex)
Fluvial - tidal transition

TDEC Tide-dominated estuary complex Southern area: S1-8

Northern area: N1-4
Log-sections: 1-30 this study
Log-sections: a-d re-produced
from Dam and Surlyk, (1998)

KSG
FTT

SHFS Shoreface-foreshore sandstone

KSG

Tide-dominated/-influenced delta platform

WIBE Wave-influenced brackish embayment

TDDP

TDDC Tide-dominated delta clinothem:

Wave-dominated brackish-marine embayment

WDBE
WDDL

0km 5km 10km

TDDF Tide-dominated pro-delta and delta-front Wave-dominated delta-lobe

TDSS Tide-dominated sub-tidal sandy shoal SORT The Sortehat Formation (Offshore transition / open-marine)

Fig. 7. The depositional architecture of the Neill Klinter Group summarised with lateral and vertical relationships of the eight allostratigraphic units (AU1
to 8) and ten architectural elements (AE) within the two major stratigraphical compartments of this study. The major unconformity separating the upper
compartment from the Sortehat Formation, or the stratigraphically next identifiable key stratal surface below, is used as a datum for correlation of measured
sections. For study localities see Fig. 4.