Ørnhøj Fm

Hodde Fm

Odderup Fm

Odderup Fm

Arnum Fm

Klintinghoved Fm

Klintinghoved Fm

Vejle Fjord Fm

Billund Fm

BillundFm

BillundFm

Billund Fm

Brejning Fm

Vejle Fjord Fm

Bastrup Fm

Bastrup Fm

Bastrup Fm

Stauning Mb

Fasteholt Mb

Addit Mb

West

East

ResenDGU no. 65.1643

MausingDGU no. 76.2013

UlfborgDGU no. 73.971Fjand

DGU no. 76.635

HolstebroDGU no. 64.1640

Clay and clayey silt

Fine-grained sand

Medium-grained sand

Coarse-grained sand

Gravel

Coal

Base Quaternary

Top Bastrup Fm / Klintinghoved Fm

Top Billund Fm / Vejle Fjord Fm

Lithology in borehole Main boundaries Depositional environments

Top Brejning Fm

Top Paleocene clay

Top Odderup Fm / Arnum Fm

Sand (marine)

Sand/gravel (continental)

Clay (marine)

Clay (lagoonal)

Shell bed

Clay (continental)

Coal

210

200

190

180

170

160

150

140

130

120

110

100

90

80

70

60

50

40

30

20

10

0m.b.s.

270270

260

250

240

230

220

210

200

190

180

170

160

150

140

130

120

110

100

90

80

70

60

50

40

30

20

10

0m.b.s.

260

250

240

230

220

210

200

190

180

170

160

150

140

130

120

110

100

90

80

70

60

50

40

30

20

10

0m.b.s.

200

190

180

170

160

150

140

130

120

110

100

90

80

70

60

50

40

30

20

10

0m.b.s.

200

190

180

170

160

150

140

130

120

110

100

90

80

70

60

50

40

30

20

10

0m.b.s.

m.b.s.

GR

GR

GR

GR

GR

GR

SorringDGU no. 88.1450

9090

100

80

70

60

50

40

30

20

10

0

Plate 5W–E-striking correlation panel from the Fjand borehole in the west to the Sorring borehole in the east. Correlation between wells is based on integra-tion of borehole (lithostratigraphy, biostratigraphy) and seismic data; sedimentary architecture between wells is based primarily on seismic data.