Dynamics of sedimentary basins and underlying lithosphere at plate boundaries: The Eastern Mediterranean
Open Access

Table 3

Model assumptions for the three typical fault regimes plotted in a 3D Mohr diagram.

Fault type Case Strike angle, α (relative to SHmax) Angle, β (normal stress relative to horizontal plane) Dip angle, θ = 90° − β
Normal fault 1 30° 60°
Strike-slip 2 30° 90°
Reverse fault 3 90° 60° 30°

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