FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3208291750> ?p ?o ?g. }

• W3208291750 endingPage "1889" @default.
• W3208291750 startingPage "1869" @default.
• W3208291750 abstract "Abstract Submarine channels are conduits for sediment delivery to continental margins, and channel deposits can be sandy components of the fill in tectonically active salt basins. Examples of salt-withdrawal basin fill commonly show successions of sandy channelized or sheet-like systems alternating with more mud-rich mass-transport complexes and hemipelagites. This alternation of depositional styles is controlled by subsidence and sediment-supply histories. Salt-basin fill comprising successions of largely uninterrupted meandering-channel deposition are less commonly recognized. This begs the questions: can sediment supply be large enough to overwhelm basin subsidence and result in a thick succession of channel deposits, and, if so, how would such a channel system evolve? Here, we use three-dimensional seismic-reflection data from a &gt;1500 km2 region with salt-influenced topography in the Campos Basin, offshore Brazil, to evaluate the influence of salt diapirs on an Upper Cretaceous–Paleogene giant meandering submarine-channel system (channel elements &gt;1 km wide; meander wavelengths several kilometers to &gt;10 km). The large scale of the channels in the Campos Basin suggests that sediment discharge was large enough to sustain the meandering channel system in spite of large variability in subsidence across the region. We interpreted 22 channel centerlines to reconstruct the detailed kinematic evolution of this depositional system; this level of detail is akin to that of recent studies of meandering fluvial channels in time-lapse Landsat satellite images. The oldest channel elements are farther from salt diapirs than many of the younger ones; the centerlines of the older channel elements exhibit a correlation between curvature and migration rate, and a spatial delay between locations of peak curvature and maximum migration distance, similar to that observed in rivers. As many of the younger channel centerlines expanded toward nearby salt diapirs, their migration pattern switched to downstream translation as a result of partial confinement. Channel segments that docked against salt diapirs became less mobile, and, as a result, they do not show a correlation between curvature and migration rate. The channel migration pattern in the Campos Basin is different compared to that of a tectonically quiescent continental rise where meander evolution is unobstructed. This style of channelized basin filling is different from that of many existing examples of salt-withdrawal minibasins that are dominated by overall less-channelized deposits. This difference might be a result of the delivery of voluminous coarse sediment and high discharge of channel-forming turbidity currents to the Campos Basin from rivers draining actively uplifting coastal mountains of southeastern Brazil. Detailed kinematic analysis of such well-preserved channels can be used to reconstruct the impact of structural deformation on basin fill." @default.
• W3208291750 created "2021-11-08" @default.
• W3208291750 creator A5035258144 @default.
• W3208291750 creator A5050095141 @default.
• W3208291750 creator A5066077357 @default.
• W3208291750 creator A5067093800 @default.
• W3208291750 date "2021-11-02" @default.
• W3208291750 modified "2023-09-27" @default.
• W3208291750 title "Giant meandering channel evolution, Campos deep-water salt basin, Brazil" @default.
• W3208291750 cites W1483157968 @default.
• W3208291750 cites W1486690691 @default.
• W3208291750 cites W1491790706 @default.
• W3208291750 cites W1579624063 @default.
• W3208291750 cites W1587869157 @default.
• W3208291750 cites W1601770134 @default.
• W3208291750 cites W1890572410 @default.
• W3208291750 cites W1897519531 @default.
• W3208291750 cites W1970130975 @default.
• W3208291750 cites W1972495539 @default.
• W3208291750 cites W1973847654 @default.
• W3208291750 cites W1976429424 @default.
• W3208291750 cites W1986943807 @default.
• W3208291750 cites W1988119980 @default.
• W3208291750 cites W1991584328 @default.
• W3208291750 cites W1992872822 @default.
• W3208291750 cites W1994760441 @default.
• W3208291750 cites W2001171989 @default.
• W3208291750 cites W2010774435 @default.
• W3208291750 cites W2011421023 @default.
• W3208291750 cites W2012533964 @default.
• W3208291750 cites W2014207951 @default.
• W3208291750 cites W2014697670 @default.
• W3208291750 cites W2021022927 @default.
• W3208291750 cites W2026886308 @default.
• W3208291750 cites W2031717934 @default.
• W3208291750 cites W2043216598 @default.
• W3208291750 cites W2045140034 @default.
• W3208291750 cites W2045286199 @default.
• W3208291750 cites W2052361848 @default.
• W3208291750 cites W2055044870 @default.
• W3208291750 cites W2056433714 @default.
• W3208291750 cites W2059950589 @default.
• W3208291750 cites W2060765669 @default.
• W3208291750 cites W2069028147 @default.
• W3208291750 cites W2071947072 @default.
• W3208291750 cites W2079277569 @default.
• W3208291750 cites W2083690047 @default.
• W3208291750 cites W2084064600 @default.
• W3208291750 cites W2087951421 @default.
• W3208291750 cites W2088361432 @default.
• W3208291750 cites W2089207774 @default.
• W3208291750 cites W2090053550 @default.
• W3208291750 cites W2092617817 @default.
• W3208291750 cites W2094209997 @default.
• W3208291750 cites W2097733376 @default.
• W3208291750 cites W2098951711 @default.
• W3208291750 cites W2103006247 @default.
• W3208291750 cites W2106103280 @default.
• W3208291750 cites W2108840758 @default.
• W3208291750 cites W2109222348 @default.
• W3208291750 cites W2112074996 @default.
• W3208291750 cites W2121593483 @default.
• W3208291750 cites W2125107304 @default.
• W3208291750 cites W2128776046 @default.
• W3208291750 cites W2132795818 @default.
• W3208291750 cites W2139762350 @default.
• W3208291750 cites W2140237976 @default.
• W3208291750 cites W2144432096 @default.
• W3208291750 cites W2150469385 @default.
• W3208291750 cites W2152858301 @default.
• W3208291750 cites W2159719357 @default.
• W3208291750 cites W2160113537 @default.
• W3208291750 cites W2324279995 @default.
• W3208291750 cites W2324662799 @default.
• W3208291750 cites W2330214195 @default.
• W3208291750 cites W2330416411 @default.
• W3208291750 cites W240743656 @default.
• W3208291750 cites W2483583879 @default.
• W3208291750 cites W2503851567 @default.
• W3208291750 cites W2515318037 @default.
• W3208291750 cites W2553219535 @default.
• W3208291750 cites W2744015449 @default.
• W3208291750 cites W2757990909 @default.
• W3208291750 cites W2764048632 @default.
• W3208291750 cites W2767645488 @default.
• W3208291750 cites W2777825638 @default.
• W3208291750 cites W2791871879 @default.
• W3208291750 cites W2793462429 @default.
• W3208291750 cites W2886963418 @default.
• W3208291750 cites W2895212784 @default.
• W3208291750 cites W2897106604 @default.
• W3208291750 cites W2914849477 @default.
• W3208291750 cites W2947364297 @default.
• W3208291750 cites W2976617628 @default.
• W3208291750 cites W3013153646 @default.
• W3208291750 cites W3019532574 @default.
• W3208291750 cites W3088747376 @default.
• W3208291750 cites W3089506537 @default.

• next