Matches in SemOpenAlex for { <https://semopenalex.org/work/W2017478854> ?p ?o ?g. }
Showing items 1 to 91 of
91
with 100 items per page.
- W2017478854 endingPage "354" @default.
- W2017478854 startingPage "339" @default.
- W2017478854 abstract "The eastern Mediterranean sedimentary regime is dominated by sediment transport from the Nile River and its delta, but recent studies have also suggested a certain contribution of clay fraction from streams to the continental shelf and slope off Israel. In the present study we focused on clay fraction deposition along the inner (∼40–1000 m water depth) shelf of Israel in order to substantiate and quantify its different sources. For this purpose detailed XRD mineralogical determinations as well as chemical compositions of the clay (<2 μm) fraction of marine and continental sediments were used. The clay mineral composition of Israeli stream sediments is variable, with no distinct spatial or temporal trend, but within a limited assemblage. This clay assemblage is made up of illite–smectite (IS) phases (70–90%), kaolinite (5–25%) and illite (<10%) and is similar to that of the Nile. However, it is clearly distinguished by the type of the IS phases, which are derived mainly from Mesozoic outcrops and recent sediments/soils and are less expandable than those of the Nile, which are derived mainly from weathered basalt. The Nile-derived component is depleted in the marine clay fraction along the Israel coast, evidenced by a decrease of IS expandability and the Fe2O3/Al2O3 ratio, and an increase in the K2O/Al2O3, MgO/Al2O3 and CaO/Al2O3 ratios. The depletion is well pronounced north of Tel Aviv, where the largest coastal plain stream flows to the sea. A northward increase of carbonates in the clay fraction, and particularly of the bioskeletal component is indicated by the ratios of MgO and Sr to CaO. The contribution of the local streams to the shallow shelf marine clay fraction is estimated to be about 50%. A minor contribution of desert dust is identified by the relative increase in kaolinite in the marine sediments south of Tel Aviv." @default.
- W2017478854 created "2016-06-24" @default.
- W2017478854 creator A5022573384 @default.
- W2017478854 creator A5063999000 @default.
- W2017478854 date "2000-07-01" @default.
- W2017478854 modified "2023-10-14" @default.
- W2017478854 title "Composition of clays along the continental shelf off Israel: contribution of the Nile versus local sources" @default.
- W2017478854 cites W188142398 @default.
- W2017478854 cites W1969795380 @default.
- W2017478854 cites W1970108402 @default.
- W2017478854 cites W1970538718 @default.
- W2017478854 cites W1982020463 @default.
- W2017478854 cites W1989687428 @default.
- W2017478854 cites W1992694954 @default.
- W2017478854 cites W1997024561 @default.
- W2017478854 cites W2003416356 @default.
- W2017478854 cites W2003691801 @default.
- W2017478854 cites W2005432933 @default.
- W2017478854 cites W2023285541 @default.
- W2017478854 cites W2024240798 @default.
- W2017478854 cites W2028232018 @default.
- W2017478854 cites W2033846141 @default.
- W2017478854 cites W2043669284 @default.
- W2017478854 cites W2093256280 @default.
- W2017478854 cites W2097707707 @default.
- W2017478854 cites W2111361481 @default.
- W2017478854 cites W2763797861 @default.
- W2017478854 doi "https://doi.org/10.1016/s0025-3227(00)00021-9" @default.
- W2017478854 hasPublicationYear "2000" @default.
- W2017478854 type Work @default.
- W2017478854 sameAs 2017478854 @default.
- W2017478854 citedByCount "57" @default.
- W2017478854 countsByYear W20174788542012 @default.
- W2017478854 countsByYear W20174788542013 @default.
- W2017478854 countsByYear W20174788542014 @default.
- W2017478854 countsByYear W20174788542015 @default.
- W2017478854 countsByYear W20174788542016 @default.
- W2017478854 countsByYear W20174788542018 @default.
- W2017478854 countsByYear W20174788542019 @default.
- W2017478854 countsByYear W20174788542020 @default.
- W2017478854 countsByYear W20174788542021 @default.
- W2017478854 countsByYear W20174788542022 @default.
- W2017478854 countsByYear W20174788542023 @default.
- W2017478854 crossrefType "journal-article" @default.
- W2017478854 hasAuthorship W2017478854A5022573384 @default.
- W2017478854 hasAuthorship W2017478854A5063999000 @default.
- W2017478854 hasConcept C111368507 @default.
- W2017478854 hasConcept C114793014 @default.
- W2017478854 hasConcept C127313418 @default.
- W2017478854 hasConcept C161509811 @default.
- W2017478854 hasConcept C17409809 @default.
- W2017478854 hasConcept C184751465 @default.
- W2017478854 hasConcept C199289684 @default.
- W2017478854 hasConcept C2779429093 @default.
- W2017478854 hasConcept C2779899878 @default.
- W2017478854 hasConcept C2816523 @default.
- W2017478854 hasConcept C40212044 @default.
- W2017478854 hasConcept C6494504 @default.
- W2017478854 hasConceptScore W2017478854C111368507 @default.
- W2017478854 hasConceptScore W2017478854C114793014 @default.
- W2017478854 hasConceptScore W2017478854C127313418 @default.
- W2017478854 hasConceptScore W2017478854C161509811 @default.
- W2017478854 hasConceptScore W2017478854C17409809 @default.
- W2017478854 hasConceptScore W2017478854C184751465 @default.
- W2017478854 hasConceptScore W2017478854C199289684 @default.
- W2017478854 hasConceptScore W2017478854C2779429093 @default.
- W2017478854 hasConceptScore W2017478854C2779899878 @default.
- W2017478854 hasConceptScore W2017478854C2816523 @default.
- W2017478854 hasConceptScore W2017478854C40212044 @default.
- W2017478854 hasConceptScore W2017478854C6494504 @default.
- W2017478854 hasIssue "3-4" @default.
- W2017478854 hasLocation W20174788541 @default.
- W2017478854 hasOpenAccess W2017478854 @default.
- W2017478854 hasPrimaryLocation W20174788541 @default.
- W2017478854 hasRelatedWork W1981721037 @default.
- W2017478854 hasRelatedWork W2028587755 @default.
- W2017478854 hasRelatedWork W2060964626 @default.
- W2017478854 hasRelatedWork W2064504981 @default.
- W2017478854 hasRelatedWork W2099951326 @default.
- W2017478854 hasRelatedWork W2128308922 @default.
- W2017478854 hasRelatedWork W2129507006 @default.
- W2017478854 hasRelatedWork W2323580660 @default.
- W2017478854 hasRelatedWork W2518549959 @default.
- W2017478854 hasRelatedWork W2902393287 @default.
- W2017478854 hasVolume "167" @default.
- W2017478854 isParatext "false" @default.
- W2017478854 isRetracted "false" @default.
- W2017478854 magId "2017478854" @default.
- W2017478854 workType "article" @default.