Manganese and phosphorite nodules form on the seafloor and are syndepositional in origin.
2.
The region has a complex basin history in terms of syndepositional deformation and superimposition of numerous episodes of fault reactivation in the basin.
3.
"' Growth faults "'are syndepositional or syn-sedimentary extensional faults that initiate and evolve at the margins of continental plates.
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