FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2082546809> ?p ?o ?g. }

• W2082546809 endingPage "2060" @default.
• W2082546809 startingPage "2045" @default.
• W2082546809 abstract "The Aegean Sea covers an area of some 160×103 km2 and receives the water/sediment fluxes from a mountainous drainage basin of >200×103 km2. On the basis of its morphodynamic characteristics, the Aegean Basin could be divided into: (1) the North Aegean Sea, an elongated region (trending between N50° and N70°) including the extensive northern shelves and the Deep Aegean Trough; (2) the Central Aegean, which includes: the Cyclades Plateau, a relatively shallow (average depth <350 m) submerged platform, surrounded by small basins (up to 1000 m depth), including also the relatively extended eastern shelf of Asia Minor, and (3) the Southern Aegean Sea, located southwards of the Hellenic volcanic arc, which presents the characteristics of a true back-arc basin (the Cretan Sea).The surficial unconsolidated sediments of the north Aegean floor are dominated by the terrigenous component (from 50% up to >90%) due to the large terrigenous riverine fluxes. The South Aegean presents high percentages (>50%) of biogenic material, due to the small terrigenous inputs and despite the fact that it is more oligotrophic than the North Aegean. The Central Aegean presents a transitional character with the terrigenous influxes being imported along its eastern part and quantitatively being in between those of the North and South Aegean Sea sub-regions.The coarse-grained materials in shallow (shelf) areas are attributed to ‘relict’ deposits, while those in large water depths are almost exclusively biogenic products. The offshore distribution of the fine-grained terrigenous material is dominated by the overall circulation pattern, while meso-scale eddies may, locally, either enhance (anticyclones) or reduce (cyclones) settling rates. Moreover, the spatial distribution of the predominant clay minerals (illite and smectite) and of kaolinite and chlorite is governed by the lithology and proximity to land source areas, the water circulation and the processes of differential settling and flocculation.Overall, the North Aegean is characterised by sedimentation processes similar to those of a ‘continental margin’, primarily neritic and secondarily hemipelagic, the Central Aegean region mostly by hemipelagic and the South Aegean, behaving more like an ‘oceanic margin’, mostly by pelagic processes." @default.
• W2082546809 created "2016-06-24" @default.
• W2082546809 creator A5091022962 @default.
• W2082546809 date "2009-09-01" @default.
• W2082546809 modified "2023-09-26" @default.
• W2082546809 title "Origin and distribution of the terrigenous component of the unconsolidated surface sediment of the Aegean floor: A synthesis" @default.
• W2082546809 cites W1589900634 @default.
• W2082546809 cites W1668250948 @default.
• W2082546809 cites W1970538718 @default.
• W2082546809 cites W1971526896 @default.
• W2082546809 cites W1972228613 @default.
• W2082546809 cites W1973967941 @default.
• W2082546809 cites W1976453166 @default.
• W2082546809 cites W1979846932 @default.
• W2082546809 cites W1980106909 @default.
• W2082546809 cites W1985378205 @default.
• W2082546809 cites W1985966928 @default.
• W2082546809 cites W1987336309 @default.
• W2082546809 cites W1989555076 @default.
• W2082546809 cites W1991506817 @default.
• W2082546809 cites W2004629382 @default.
• W2082546809 cites W2007005187 @default.
• W2082546809 cites W2009108673 @default.
• W2082546809 cites W2014449029 @default.
• W2082546809 cites W2016576584 @default.
• W2082546809 cites W2018720527 @default.
• W2082546809 cites W2019081382 @default.
• W2082546809 cites W2022259824 @default.
• W2082546809 cites W2022944614 @default.
• W2082546809 cites W2024210515 @default.
• W2082546809 cites W2024606848 @default.
• W2082546809 cites W2024788395 @default.
• W2082546809 cites W2025484526 @default.
• W2082546809 cites W2027055361 @default.
• W2082546809 cites W2030466717 @default.
• W2082546809 cites W2030769041 @default.
• W2082546809 cites W2032281540 @default.
• W2082546809 cites W2033846141 @default.
• W2082546809 cites W2034585153 @default.
• W2082546809 cites W2034657844 @default.
• W2082546809 cites W2035001758 @default.
• W2082546809 cites W2035687132 @default.
• W2082546809 cites W2037393819 @default.
• W2082546809 cites W2037778413 @default.
• W2082546809 cites W2042203476 @default.
• W2082546809 cites W2042458403 @default.
• W2082546809 cites W2043490045 @default.
• W2082546809 cites W2043662008 @default.
• W2082546809 cites W2044591694 @default.
• W2082546809 cites W2044913996 @default.
• W2082546809 cites W2045052076 @default.
• W2082546809 cites W2048496597 @default.
• W2082546809 cites W2053957590 @default.
• W2082546809 cites W2057526825 @default.
• W2082546809 cites W2058730552 @default.
• W2082546809 cites W2060731524 @default.
• W2082546809 cites W2061847384 @default.
• W2082546809 cites W2065366941 @default.
• W2082546809 cites W2065664616 @default.
• W2082546809 cites W2065752147 @default.
• W2082546809 cites W2066073215 @default.
• W2082546809 cites W2066204794 @default.
• W2082546809 cites W2066893720 @default.
• W2082546809 cites W2069033727 @default.
• W2082546809 cites W2070384618 @default.
• W2082546809 cites W2070635567 @default.
• W2082546809 cites W2074924591 @default.
• W2082546809 cites W2081198055 @default.
• W2082546809 cites W2081472723 @default.
• W2082546809 cites W2081807722 @default.
• W2082546809 cites W2082502699 @default.
• W2082546809 cites W2084362661 @default.
• W2082546809 cites W2088753902 @default.
• W2082546809 cites W2089061324 @default.
• W2082546809 cites W2089111492 @default.
• W2082546809 cites W2089268227 @default.
• W2082546809 cites W2091610352 @default.
• W2082546809 cites W2093998546 @default.
• W2082546809 cites W2103548190 @default.
• W2082546809 cites W2110481623 @default.
• W2082546809 cites W2114367951 @default.
• W2082546809 cites W2132557089 @default.
• W2082546809 cites W2132867586 @default.
• W2082546809 cites W2142711185 @default.
• W2082546809 cites W2143426536 @default.
• W2082546809 cites W2152217615 @default.
• W2082546809 cites W2156536539 @default.
• W2082546809 cites W2160485438 @default.
• W2082546809 cites W2171483221 @default.
• W2082546809 cites W2342344255 @default.
• W2082546809 cites W3137814049 @default.
• W2082546809 doi "https://doi.org/10.1016/j.csr.2008.11.010" @default.
• W2082546809 hasPublicationYear "2009" @default.
• W2082546809 type Work @default.
• W2082546809 sameAs 2082546809 @default.
• W2082546809 citedByCount "33" @default.
• W2082546809 countsByYear W20825468092012 @default.
• W2082546809 countsByYear W20825468092013 @default.

• next