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• W2898827013 abstract "Abstract Sediment waves are commonly observed on the sea floor and often vary in morphology and geometry according to factors such as seabed slope, density and discharge of turbidity currents, and the presence of persistent contour currents. This paper documents the morphology, internal geometry and distribution of deep‐water (4000 to 5000 m) bedforms observed on the sea floor offshore eastern Canada using high‐resolution multibeam bathymetry data and seismic stratigraphy. The bedforms have wavelengths of >1 km but fundamentally vary in terms of morphology and internal stratigraphy, and are distinguished into three main types. The first type, characterized by their long‐wavelength crescentic shape, is interpreted as net‐erosional cyclic steps. These cyclic steps were formed by turbidity currents flowing through canyons and overtopping and breaching levées. The second type, characterized by their linear shape and presence on levées, is interpreted as net‐depositional cyclic steps. These upslope migrating bedforms are strongly aggradational, indicating high sediment deposition from turbidity currents. The third type, characterized by their obliqueness to canyons, is observed on an open slope and is interpreted as antidunes. These antidunes were formed by the deflection of the upper dilute, low‐density parts of turbidity currents by contour currents. The modelling of the behaviour of these different types of turbidity currents reveals that fast‐flowing flows form cyclic steps while their upper parts overspill and are entrained westward by contour currents. The interaction between turbidity currents and contour currents results in flow thickening and reduced sediment concentration, which leads to lower flow velocities. Lower velocities, in turn, allow the formation of antidunes instead of cyclic steps because the densiometric Froude number (Fr′) decreases. Therefore, this study shows that both net‐erosional and net‐depositional cyclic steps are distributed along channels where turbidity currents prevail whereas antidunes form on open slopes, in a mixed turbidite/contourite system. This study provides insights into the influence of turbidity currents versus contour currents on the morphology, geometry and distribution of bedforms in a mixed turbidite–contourite system." @default.
• W2898827013 created "2018-11-09" @default.
• W2898827013 creator A5009427879 @default.
• W2898827013 creator A5032913391 @default.
• W2898827013 creator A5074035099 @default.
• W2898827013 date "2019-02-19" @default.
• W2898827013 modified "2023-10-14" @default.
• W2898827013 title "The influence of turbidity currents and contour currents on the distribution of deep‐water sediment waves offshore eastern Canada" @default.
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• W2898827013 cites W1969804499 @default.
• W2898827013 cites W1977721779 @default.
• W2898827013 cites W1982645341 @default.
• W2898827013 cites W1986132337 @default.
• W2898827013 cites W1992867679 @default.
• W2898827013 cites W1998907201 @default.
• W2898827013 cites W2005617902 @default.
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• W2898827013 cites W2014603107 @default.
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• W2898827013 cites W2024610996 @default.
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• W2898827013 doi "https://doi.org/10.1111/sed.12557" @default.
• W2898827013 hasPublicationYear "2019" @default.
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