FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2804546437> ?p ?o ?g. }

• W2804546437 endingPage "138" @default.
• W2804546437 startingPage "123" @default.
• W2804546437 abstract "In this study, analyses of a high-resolution, three-dimensional seismic reflection dataset and well-log data were combined to characterise a distinct Pliocene interval in the Levant Basin offshore central Israel. This succession is characterised by moderate to high-amplitude, discontinuous to continuous seismic reflections between a mass transport deposit above and an undeformed basin series below. The studied interval contains two separate channelised subunits, which predated the salt related deformations. Morphologically, the channels trend in a north to northwest direction, are incised <50 m, are ~50 m to 350 m wide and increase in number from base to top. A vertical variation in channel morphology style and stratigraphic organization is identified. The lower part of each subunit is dominated by coarser grained, narrow V-shaped channels (average width <120 m and low sinuosity, <1.06). In contrast, the upper part of each subunit is predominantly fine-grained and U-shaped with relatively wide channels (average width >230 m and higher sinuosity, >1.1). The mechanisms that control the interplay between sedimentary processes and channel evolution show a cyclic pattern. Due to the cyclic occurrence of different channel types and the estimated age of the studied interval, formation and evolutionary processes of the submarine channels in the study area are likely to be controlled by relative sea level fluctuations and increased Nile River sediment supply, which is associated with rapid uplift of the Ethiopian plateau and increased African Monsoon rainfall during the Pliocene." @default.
• W2804546437 created "2018-06-01" @default.
• W2804546437 creator A5006028315 @default.
• W2804546437 creator A5011927280 @default.
• W2804546437 creator A5025494007 @default.
• W2804546437 creator A5065226808 @default.
• W2804546437 creator A5078588753 @default.
• W2804546437 creator A5078612470 @default.
• W2804546437 date "2018-09-01" @default.
• W2804546437 modified "2023-10-14" @default.
• W2804546437 title "Seismic geomorphology of submarine channel-belt complexes in the Pliocene of the Levant Basin, offshore central Israel" @default.
• W2804546437 cites W1180057341 @default.
• W2804546437 cites W1483157968 @default.
• W2804546437 cites W1528044173 @default.
• W2804546437 cites W1649050783 @default.
• W2804546437 cites W1963556352 @default.
• W2804546437 cites W1965430736 @default.
• W2804546437 cites W1970193144 @default.
• W2804546437 cites W1970259090 @default.
• W2804546437 cites W1972495539 @default.
• W2804546437 cites W1972621712 @default.
• W2804546437 cites W1973309627 @default.
• W2804546437 cites W1973847654 @default.
• W2804546437 cites W1978082161 @default.
• W2804546437 cites W1979381341 @default.
• W2804546437 cites W1981532054 @default.
• W2804546437 cites W1984273256 @default.
• W2804546437 cites W1991468612 @default.
• W2804546437 cites W1992855123 @default.
• W2804546437 cites W1992872822 @default.
• W2804546437 cites W1994760441 @default.
• W2804546437 cites W1995263625 @default.
• W2804546437 cites W1995854523 @default.
• W2804546437 cites W2003820922 @default.
• W2804546437 cites W2006004526 @default.
• W2804546437 cites W2006185800 @default.
• W2804546437 cites W2008205524 @default.
• W2804546437 cites W2011899563 @default.
• W2804546437 cites W2013276923 @default.
• W2804546437 cites W2014318045 @default.
• W2804546437 cites W2014565040 @default.
• W2804546437 cites W2014697670 @default.
• W2804546437 cites W2019967542 @default.
• W2804546437 cites W2021022927 @default.
• W2804546437 cites W2025296492 @default.
• W2804546437 cites W2026490718 @default.
• W2804546437 cites W2027848502 @default.
• W2804546437 cites W2032363988 @default.
• W2804546437 cites W2040558728 @default.
• W2804546437 cites W2040750529 @default.
• W2804546437 cites W2040832270 @default.
• W2804546437 cites W2040964459 @default.
• W2804546437 cites W2040989064 @default.
• W2804546437 cites W2043075830 @default.
• W2804546437 cites W2048084380 @default.
• W2804546437 cites W2049070534 @default.
• W2804546437 cites W2049328822 @default.
• W2804546437 cites W2052361848 @default.
• W2804546437 cites W2055344849 @default.
• W2804546437 cites W2063272166 @default.
• W2804546437 cites W2063333127 @default.
• W2804546437 cites W2066785522 @default.
• W2804546437 cites W2072621765 @default.
• W2804546437 cites W2077286486 @default.
• W2804546437 cites W2086046118 @default.
• W2804546437 cites W2086738712 @default.
• W2804546437 cites W2087951421 @default.
• W2804546437 cites W2087959768 @default.
• W2804546437 cites W2089207774 @default.
• W2804546437 cites W2090053550 @default.
• W2804546437 cites W2091462783 @default.
• W2804546437 cites W2092885778 @default.
• W2804546437 cites W2096831672 @default.
• W2804546437 cites W2097733376 @default.
• W2804546437 cites W2100255021 @default.
• W2804546437 cites W2100821992 @default.
• W2804546437 cites W2103006247 @default.
• W2804546437 cites W2104828276 @default.
• W2804546437 cites W2113282539 @default.
• W2804546437 cites W2114216018 @default.
• W2804546437 cites W2119077761 @default.
• W2804546437 cites W2120162798 @default.
• W2804546437 cites W2130432031 @default.
• W2804546437 cites W2130489480 @default.
• W2804546437 cites W2132232793 @default.
• W2804546437 cites W2133947842 @default.
• W2804546437 cites W2139762350 @default.
• W2804546437 cites W2140042990 @default.
• W2804546437 cites W2142644050 @default.
• W2804546437 cites W2147422283 @default.
• W2804546437 cites W2148169148 @default.
• W2804546437 cites W2151250266 @default.
• W2804546437 cites W2160113537 @default.
• W2804546437 cites W2210992848 @default.
• W2804546437 cites W2304278701 @default.
• W2804546437 cites W2317723920 @default.
• W2804546437 cites W2344989047 @default.
• W2804546437 cites W2347169772 @default.

• next