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Table 2 Depth difference between actual well tops of wells within the AOI and modeled stratigraphic tops

From: RETRACTED ARTICLE: Predictability and controlling factors of overpressure in the North Alpine Foreland Basin, SE Germany: an interdisciplinary post-drill analysis of the Geretsried GEN-1 deep geothermal well

 

Well A (m)

Well B (m)

Well C (m)

Well D (m)

B2 (m)

B4 (m)

B7 (m)

B12 (m)

Quarternary

0

9

1

33

− 2

1

4

− 5

OSM

0

12

10

− 7

1

− 1

7

− 2

Burdigalian

− 3

23

− 14

17

2

− 10

− 1

− 5

Aquitanian

− 6

12

− 36

34

− 2

− 6

− 12

− 5

Chattian

1

7

− 17

20

− 5

− 6

− 11

1

Rupelian

4

6

− 21

70

6

− 4

19

− 9

Sannoisian

13

− 24

− 7

18

− 1

n/a

1

26

Eocene

13

− 25

− 10

30

n/a

n/a

− 7

27

U. Cretaceous

n/a

− 26

− 12

35

n/a

n/a

− 1

22

L. Cretaceous

14

− 27

n/a

51

− 1

n/a

− 13

14

Jurassic

11

− 30

n/a

56

5

n/a

n/a

34