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• W2158420108 endingPage "113" @default.
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• W2158420108 abstract "Based upon 2D reflection seismic data and numerical modelling, this study confirms the presence of a complex deep-water sedimentary system on the present-day seafloor at the intersection of the Xisha Trough and the Northwest Sub-Basin (South China Sea) and investigates their relationship with bottom currents. The deep-water sedimentary system consists of submarine canyons, slides and slumps, wave-like successions, mounded drifts and two groups of marginal depressions (those with erosional features and those appearing as morphological sediment sinks). Three-dimensional process-based modelling is applied to investigate sediment dynamics induced by a combined effect of tidal currents and a quasi-steady geostrophic current (South China Sea Deep Water Circulation). Simulation results show that the South China Sea Deep Water Circulation at the southeastern flank of the seamount plateau could reach velocities of 15 cm/s during flood tides, enabling erosion and transport processes. In contrast, the rest of the plateau area is favoured for deposition, since current velocities in this region are persistently lower than 10 cm/s. The current velocities at the feet of the obstacles (where the morphological depressions are located) are strengthened and are several cm/s higher than that in adjacent flat areas (e.g. where the mounded drifts are located). The flow is constricted and accelerated after being deflected by the obstacles, resulting in contrasting higher sedimentation rates within the mounded sediments and lower rates at the morphological depressions. A comparison between the seismic stratigraphy and the simulated fluid dynamics enables a decoding of the pathway, identifying the current regime as well as unravelling the relationship between depositional processes and the deep-sea water circulation. This study provides new insights and exposes new challenges in understanding the dynamics of deep-sea sedimentation processes in South China Sea." @default.
• W2158420108 created "2016-06-24" @default.
• W2158420108 creator A5004932817 @default.
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• W2158420108 creator A5076687485 @default.
• W2158420108 date "2016-08-01" @default.
• W2158420108 modified "2023-10-12" @default.
• W2158420108 title "Deep-water sedimentary systems and their relationship with bottom currents at the intersection of Xisha Trough and Northwest Sub-Basin, South China Sea" @default.
• W2158420108 cites W1508700254 @default.
• W2158420108 cites W1529498661 @default.
• W2158420108 cites W1770855718 @default.
• W2158420108 cites W1822282223 @default.
• W2158420108 cites W1850172458 @default.
• W2158420108 cites W1852502153 @default.
• W2158420108 cites W1965005715 @default.
• W2158420108 cites W1970883070 @default.
• W2158420108 cites W1971381690 @default.
• W2158420108 cites W1974922958 @default.
• W2158420108 cites W1975360061 @default.
• W2158420108 cites W1976182169 @default.
• W2158420108 cites W1977518148 @default.
• W2158420108 cites W1978223193 @default.
• W2158420108 cites W1978928221 @default.
• W2158420108 cites W1984646336 @default.
• W2158420108 cites W1986417585 @default.
• W2158420108 cites W1987347959 @default.
• W2158420108 cites W1988661126 @default.
• W2158420108 cites W1992872822 @default.
• W2158420108 cites W1995016348 @default.
• W2158420108 cites W1996415129 @default.
• W2158420108 cites W1999867277 @default.
• W2158420108 cites W2001332003 @default.
• W2158420108 cites W2001546944 @default.
• W2158420108 cites W2001770705 @default.
• W2158420108 cites W2002775898 @default.
• W2158420108 cites W2003450165 @default.
• W2158420108 cites W2006854942 @default.
• W2158420108 cites W2013591853 @default.
• W2158420108 cites W2013675212 @default.
• W2158420108 cites W2014124878 @default.
• W2158420108 cites W2014167742 @default.
• W2158420108 cites W2014697670 @default.
• W2158420108 cites W2025280725 @default.
• W2158420108 cites W2027837291 @default.
• W2158420108 cites W2030675100 @default.
• W2158420108 cites W2039955240 @default.
• W2158420108 cites W2043313420 @default.
• W2158420108 cites W2043942893 @default.
• W2158420108 cites W2049123085 @default.
• W2158420108 cites W2050915907 @default.
• W2158420108 cites W2054107889 @default.
• W2158420108 cites W2055227112 @default.
• W2158420108 cites W2058039750 @default.
• W2158420108 cites W2061713545 @default.
• W2158420108 cites W2064411185 @default.
• W2158420108 cites W2064558996 @default.
• W2158420108 cites W2066680516 @default.
• W2158420108 cites W2069086849 @default.
• W2158420108 cites W2071003117 @default.
• W2158420108 cites W2073055132 @default.
• W2158420108 cites W2075015194 @default.
• W2158420108 cites W2075142898 @default.
• W2158420108 cites W2077474441 @default.
• W2158420108 cites W2079383600 @default.
• W2158420108 cites W2079568162 @default.
• W2158420108 cites W2084269307 @default.
• W2158420108 cites W2084475884 @default.
• W2158420108 cites W2087258637 @default.
• W2158420108 cites W2091196667 @default.
• W2158420108 cites W2092015985 @default.
• W2158420108 cites W2092606366 @default.
• W2158420108 cites W2099905921 @default.
• W2158420108 cites W2110312429 @default.
• W2158420108 cites W2118334264 @default.
• W2158420108 cites W2122826546 @default.
• W2158420108 cites W2130015685 @default.
• W2158420108 cites W2132216138 @default.
• W2158420108 cites W2134121330 @default.
• W2158420108 cites W2134778087 @default.
• W2158420108 cites W2137297774 @default.
• W2158420108 cites W2139245050 @default.
• W2158420108 cites W2141861439 @default.
• W2158420108 cites W2142396396 @default.
• W2158420108 cites W2145576101 @default.
• W2158420108 cites W2145619152 @default.
• W2158420108 cites W2148362593 @default.
• W2158420108 cites W2151920552 @default.
• W2158420108 cites W2158219765 @default.
• W2158420108 cites W2177458655 @default.
• W2158420108 cites W2183306449 @default.
• W2158420108 cites W2400296767 @default.
• W2158420108 cites W71922395 @default.
• W2158420108 doi "https://doi.org/10.1016/j.margeo.2015.11.002" @default.
• W2158420108 hasPublicationYear "2016" @default.

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