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

Table 1

Fault geometries including strike orientation and dipping angles determined in the modelling process.

Fault Structural fault interpretation Strike azimuth angle relative to North Dip angle, θ Angle β = 90° − θ
A Normal fault 317° 57° 33°
B Normal fault 317° 58° 32°
C Reverse fault 44° 66° 24°
D Reverse fault 58° 66° 24°
E Normal fault 141° 61° 29°
F Normal fault 135° 54° 36°
G Normal fault 132° 72° 18°
H Normal fault 300° 74° 16°

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