FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3081285540> ?p ?o ?g. }

• W3081285540 endingPage "104531" @default.
• W3081285540 startingPage "104531" @default.
• W3081285540 abstract "The clay mineralogy and Sr-Nd isotopic composition of sediments collected in the northwestern South China Sea (SCS) were investigated to understand sediment provenance and changes in the SCS since the Late Pleistocene. Our results show that the clay mineral assemblages of the surface sediments are characterized by high amounts of illite and smectite, and low amounts of kaolinite and chlorite. The 87Sr/86Sr ratios of the surface sediments vary from 0.709617 to 0.734416, and εNd values range from −11.6 to −8.3. The clay minerals and Sr-Nd isotope records suggest that sediments in the northwestern SCS are derived from multiple sources. The sediments deposited in the eastern shelf offshore of Hainan originate predominantly from Hainan Island and South China, whereas sediments in the western shelf offshore of Hainan are derived mainly from Indochina and Hainan Island. However, sediment source and transport mechanisms in the northwestern slope of the SCS are more complicated. Our results suggest that input from the west may be the major sediment source, but regions in the east (Taiwan and Luzon) also contribute part of the terrigenous materials. Downcore variations of Sr-Nd isotopic composition in core sediments show clear glacial–interglacial fluctuations. Higher 87Sr/86Sr ratios occur during glacial period, indicating that the input of terrigenous materials from old continental rocks becomes one of the important sediment sources during these periods. The exposure of continental shelf and southward migration of the coastline during the glacial sea-level lowstand led to an increase of terrigenous supply to the northwestern slope of the SCS. The paleo-Red River and Indochina are also potentially important contributors." @default.
• W3081285540 created "2020-09-01" @default.
• W3081285540 creator A5009858362 @default.
• W3081285540 creator A5045175743 @default.
• W3081285540 creator A5059553859 @default.
• W3081285540 creator A5059922337 @default.
• W3081285540 creator A5077327850 @default.
• W3081285540 date "2020-10-01" @default.
• W3081285540 modified "2023-10-17" @default.
• W3081285540 title "Clay minerals, Sr-Nd isotopes and provenance of sediments in the northwestern South China Sea" @default.
• W3081285540 cites W1017906914 @default.
• W3081285540 cites W1169480393 @default.
• W3081285540 cites W1615944818 @default.
• W3081285540 cites W1770855718 @default.
• W3081285540 cites W1891225341 @default.
• W3081285540 cites W1935059050 @default.
• W3081285540 cites W1965536973 @default.
• W3081285540 cites W1967838752 @default.
• W3081285540 cites W1969699502 @default.
• W3081285540 cites W1970108402 @default.
• W3081285540 cites W1976680888 @default.
• W3081285540 cites W1979376249 @default.
• W3081285540 cites W1981230700 @default.
• W3081285540 cites W1986025435 @default.
• W3081285540 cites W1989193940 @default.
• W3081285540 cites W1991232829 @default.
• W3081285540 cites W1992846059 @default.
• W3081285540 cites W1993463767 @default.
• W3081285540 cites W1993814007 @default.
• W3081285540 cites W1995613661 @default.
• W3081285540 cites W1995642042 @default.
• W3081285540 cites W1996569500 @default.
• W3081285540 cites W1996849400 @default.
• W3081285540 cites W1997333129 @default.
• W3081285540 cites W2003767587 @default.
• W3081285540 cites W2007451536 @default.
• W3081285540 cites W2013430677 @default.
• W3081285540 cites W2016170233 @default.
• W3081285540 cites W2017024367 @default.
• W3081285540 cites W2018248405 @default.
• W3081285540 cites W2025901524 @default.
• W3081285540 cites W2026422386 @default.
• W3081285540 cites W2034670546 @default.
• W3081285540 cites W2041492958 @default.
• W3081285540 cites W2042365127 @default.
• W3081285540 cites W2042417616 @default.
• W3081285540 cites W2048540932 @default.
• W3081285540 cites W2049468624 @default.
• W3081285540 cites W2050399485 @default.
• W3081285540 cites W2052446941 @default.
• W3081285540 cites W2052862313 @default.
• W3081285540 cites W2053028899 @default.
• W3081285540 cites W2061898270 @default.
• W3081285540 cites W2074379113 @default.
• W3081285540 cites W2075756042 @default.
• W3081285540 cites W2076566162 @default.
• W3081285540 cites W2090705747 @default.
• W3081285540 cites W2094413158 @default.
• W3081285540 cites W2097526162 @default.
• W3081285540 cites W2099035636 @default.
• W3081285540 cites W2099251924 @default.
• W3081285540 cites W2103600357 @default.
• W3081285540 cites W2110163415 @default.
• W3081285540 cites W2112669114 @default.
• W3081285540 cites W2115454914 @default.
• W3081285540 cites W2115594328 @default.
• W3081285540 cites W2116921785 @default.
• W3081285540 cites W2120970192 @default.
• W3081285540 cites W2122118297 @default.
• W3081285540 cites W2149740141 @default.
• W3081285540 cites W2154572728 @default.
• W3081285540 cites W2169415627 @default.
• W3081285540 cites W2245675087 @default.
• W3081285540 cites W2262634775 @default.
• W3081285540 cites W2333234644 @default.
• W3081285540 cites W2338976053 @default.
• W3081285540 cites W2400665719 @default.
• W3081285540 cites W2400846228 @default.
• W3081285540 cites W2536766660 @default.
• W3081285540 cites W2618719090 @default.
• W3081285540 cites W2687058681 @default.
• W3081285540 cites W2770628460 @default.
• W3081285540 cites W2781917121 @default.
• W3081285540 cites W2782269331 @default.
• W3081285540 cites W2922216511 @default.
• W3081285540 cites W2972776850 @default.
• W3081285540 cites W2973231363 @default.
• W3081285540 cites W3149453667 @default.
• W3081285540 cites W4247165743 @default.
• W3081285540 cites W4249751050 @default.
• W3081285540 doi "https://doi.org/10.1016/j.jseaes.2020.104531" @default.
• W3081285540 hasPublicationYear "2020" @default.
• W3081285540 type Work @default.
• W3081285540 sameAs 3081285540 @default.
• W3081285540 citedByCount "12" @default.
• W3081285540 countsByYear W30812855402022 @default.
• W3081285540 countsByYear W30812855402023 @default.
• W3081285540 crossrefType "journal-article" @default.

• next