2022
DOI: 10.1016/j.marpetgeo.2022.105865
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Seismic geomorphology of a Late Cretaceous submarine channel system in the Kribi/Campo sub-basin, offshore Cameroon

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Cited by 5 publications
(2 citation statements)
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“…These factors also control turbidity current courses and volumes. The creation of turbidite reservoirs is greatly facilitated by the existence of sediment bypasses and submarine canyons [93] [94] [95]. Climatic changes and sea-level fluctuations play vital roles in the regulation of turbidite systems [96].…”
Section: Factors Influencing Turbidite System Formationmentioning
confidence: 99%
“…These factors also control turbidity current courses and volumes. The creation of turbidite reservoirs is greatly facilitated by the existence of sediment bypasses and submarine canyons [93] [94] [95]. Climatic changes and sea-level fluctuations play vital roles in the regulation of turbidite systems [96].…”
Section: Factors Influencing Turbidite System Formationmentioning
confidence: 99%
“…The Kribi-Campo sub-basin is a segment of the Cameroon Atlantic Basin, which is the southeast part of the Cameroon Atlantic Margin (CAM) located in the Gulf of Guinea (Figure 1). Previous studies explored the geoscientific and hydrocarbon aspects of the basin [1][2][3][4][5][6][7][8][9][10][11][12][13][14][15]. The offshore deepwater domain of the Kribi-Campo sub-basin is covered by up to a 5 km thick sedimentary fill [3,[6][7][8].…”
Section: Introductionmentioning
confidence: 99%