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1. Graben systems are characterized by normal faulting that forms rotational fault blocks and thin-skinned tectonics. Sediment routing in graben basins is controlled by fault patterns and interactions. 2. Maximum displacement occurs in the center of faults and decreases towards the tips, controlling the creation of accommodation space in the hanging wall basins over time. 3. As faults grow laterally and link up, the rate of tectonic subsidence and basin deepening increases, resulting in characteristic th

Author

bobecawe

Language

EN