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3-D seismic reflection data has enabled the documentation of a system of remarkable modern and buried u-shaped gullies which intimately co-exist with upslope migrating sediment waves along 80km of the Gabon continental slope. The modern gullies occur on a silty mud-dominated slope in water depths of 150–1500m on an ~50km wide slope with a gradient of 4.5° decreasing to 1.5°. The gully sets persist...
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