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Salt-driven, thin-skinned tectonics and inherited deep seated fault-driven thick tectonics in the Dezful Embayment (Zagros, Iran), illustrated by regional 2D geomechanical restoration

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Academic year: 2020

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Figure

Figure 2. Location of 2D seismic lines. Lines 75213 and 75211 have been converted to depth.
Figure 4. Reconstruction of kinematic evolution of salt driven fold propagation fault by structural inversion controlled by an inherit- inherit-ed deep-seatinherit-ed fault system

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