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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From: RETRACTED ARTICLE: Predictability and controlling factors of overpressure in the North Alpine Foreland Basin, SE Germany: an interdisciplinary post-drill analysis of the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)
Quarternary09133− 214− 5
OSM01210− 71− 17− 2
Burdigalian− 323− 14172− 10− 1− 5
Aquitanian− 612− 3634− 2− 6− 12− 5
Chattian17− 1720− 5− 6− 111
Rupelian46− 21706− 419− 9
Sannoisian13− 24− 718− 1n/a126
Eocene13− 25− 1030n/an/a− 727
U. Cretaceousn/a− 26− 1235n/an/a− 122
L. Cretaceous14− 27n/a51− 1n/a− 1314
Jurassic11− 30n/a565n/an/a34