Science – Society – Technology
From: Inferring the in situ stress regime in deep sediments: an example from the Bruchsal geothermal site
Well | Depth interval (MD) | Orientation ofSHmax | Stratigraphic formation |
---|---|---|---|
GB1 | 1,650 to 1,700 m | N 104° E | Middle Muschelkalk and Upper Buntsandstein |
1,700 to 1,775 m | N 137° E | Middle Buntsandstein | |
1,775 to 1,850 m | N 142° E | Middle Buntsandstein | |
1,850 to 1,900 m | N 145° E | Lower Buntsandstein and Upper Permian | |
GB2 | 2,026 to 2,070 m | N 090° E | Middle Keuper |
2,070 to 2,130 m | N 163° E | Lower Keuper | |
2,130 to 2,230 m | N 125° E | Upper Muschelkalk and Upper Buntsandstein | |
2,250 to 2,328 m | N 125° E | Middle Buntsandstein | |
2,330 to 2,385 m | N 145° E | Middle Buntsandstein and Upper Permian | |
2,385 to 2,475 m | N 131° E | Upper Permian | |
2,475 to 2,535 m | N 128° E | Upper Permian |