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.
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