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 304

Chlorite

Qz

Qz

Qz

epoxy

Qz

Qz

Qz

Qz

Glauco nite

Qz

Qz

Chlorite

0.5mm

Qz

0.5mm

0.5mm

(D)

Locality N4
section 29

AU AE

15 m

10

5

0 m

FMC VC

VF

Clay Silt

Gravel

Sand

Mudstone Siltstone Sandstone

(E)

170 m

AU AE

Locality N1
section 18 AU7 WDDL

Figs. E and B

165m

160 m

Mudstone Siltstone Sandstone

VF FMC VC

Clay Silt Gravel

Sand

Fig. 6. Petrographic thin-section photos show (A) chlorite-coated quartz grains; (B) glauconite between clastic quartz
grains; and (C) iron-ooids in quartz-rich sandstone in the northern study area. (D) Photo and detailed sedimentary log show
the stratigraphical occurrence of beds rich in iron-ooids at locality N4 (measured section 29). (E) A sedimentary log and
photo of glauconite-rich sandstone facies and its stratigraphical occurrence at locality N1 (measured section 18). For locali-