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This chapter discusses the spatial and temporal evolution of the sediment erosion and catchment in various strike-slip fault-related and transform margin-related settings. It documents that their study requires the use of 3D seismic imaging tied to a large number of wells, instead of a grid of reflection seismic profiles tied to wells. The chapter also focuses on the effects of tectonics and climatic forcing on the aforementioned deposition. Supporting studies include seismic- and well-based ones and studies constrained by millennium-scale continental margin deep-sea depositional rates and activity of sediment feeder systems.
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