FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2922216511> ?p ?o ?g. }

• W2922216511 endingPage "36" @default.
• W2922216511 startingPage "27" @default.
• W2922216511 abstract "Clay minerals are significant indicators that can be used to identify sources and transport patterns of both fluvial and marine sediments. The Ganges, Brahmaputra, and Surma-Meghna (SM) rivers are the most important rivers of the Bengal Basin (BB), loading a large amount of sediments from the Himalayas into the Bay of Bengal. Clay minerals of 132 surface sediment samples from the Ganges-Brahmaputra-Meghna (GBM) river system have been analyzed with X-ray diffraction (XRD) to show the variation of clay mineral assemblages in the sediments from upstream to downstream for the major rivers of the BB and to verify the validity of clay minerals as an important index for sediment provenance in the Bay of Bengal after these sediments are discharged into the neighboring seas. The results show that the clay mineral assemblage in the GBM river system consists dominantly of illite (average 66%), with smaller amounts of smectite, kaolinite, and chlorite (8%, 8%, and 17%, respectively). Smectite is diagnostic in the Ganges River sediments, with a higher content (23%) than that in the Brahmaputra (2%) and the SM River (1%); however, chlorite (21%) is high in the SM River sediments and the Brahmaputra River sediments have a high illite percentage (77%). Downstream, the smectite percentages in the Ganges River increase significantly, but the kaolinite percentages in sediments of the SM River increase slightly. Due to the continuous mixture of first the Brahmaputra River and then the SM River discharge, the clay mineral assemblages of this river system's sediments change greatly, e.g., smectite percentages decrease from 23% in the Ganges River to 8% in the GBM River via the stretch with 12% in the Ganges-Brahmaputra confluence river." @default.
• W2922216511 created "2019-03-22" @default.
• W2922216511 creator A5006674850 @default.
• W2922216511 creator A5009584320 @default.
• W2922216511 creator A5029123923 @default.
• W2922216511 creator A5069009768 @default.
• W2922216511 creator A5073938095 @default.
• W2922216511 creator A5087333416 @default.
• W2922216511 date "2019-06-01" @default.
• W2922216511 modified "2023-10-18" @default.
• W2922216511 title "Clay mineral compositions in surface sediments of the Ganges-Brahmaputra-Meghna river system of Bengal Basin, Bangladesh" @default.
• W2922216511 cites W1542705297 @default.
• W2922216511 cites W1963616190 @default.
• W2922216511 cites W1967838752 @default.
• W2922216511 cites W1970108402 @default.
• W2922216511 cites W1970637390 @default.
• W2922216511 cites W1983410167 @default.
• W2922216511 cites W1991232829 @default.
• W2922216511 cites W1993045044 @default.
• W2922216511 cites W1993814007 @default.
• W2922216511 cites W1993959112 @default.
• W2922216511 cites W1996785461 @default.
• W2922216511 cites W1999448328 @default.
• W2922216511 cites W2001908936 @default.
• W2922216511 cites W2007241988 @default.
• W2922216511 cites W2014782855 @default.
• W2922216511 cites W2016503290 @default.
• W2922216511 cites W2021595267 @default.
• W2922216511 cites W2026723150 @default.
• W2922216511 cites W2026886308 @default.
• W2922216511 cites W2039184285 @default.
• W2922216511 cites W2042685969 @default.
• W2922216511 cites W2048681680 @default.
• W2922216511 cites W2055221583 @default.
• W2922216511 cites W2059590151 @default.
• W2922216511 cites W2059906025 @default.
• W2922216511 cites W2061451164 @default.
• W2922216511 cites W2080458803 @default.
• W2922216511 cites W2089182212 @default.
• W2922216511 cites W2093278793 @default.
• W2922216511 cites W2105139056 @default.
• W2922216511 cites W2120970192 @default.
• W2922216511 cites W2134146869 @default.
• W2922216511 cites W2148505908 @default.
• W2922216511 cites W2157956461 @default.
• W2922216511 cites W2158113457 @default.
• W2922216511 cites W2166813482 @default.
• W2922216511 cites W2379575996 @default.
• W2922216511 cites W2518791735 @default.
• W2922216511 cites W2536766660 @default.
• W2922216511 cites W2602917371 @default.
• W2922216511 cites W2728636083 @default.
• W2922216511 cites W2736927917 @default.
• W2922216511 cites W2753110710 @default.
• W2922216511 cites W2771330630 @default.
• W2922216511 cites W2888681125 @default.
• W2922216511 doi "https://doi.org/10.1016/j.margeo.2019.03.007" @default.
• W2922216511 hasPublicationYear "2019" @default.
• W2922216511 type Work @default.
• W2922216511 sameAs 2922216511 @default.
• W2922216511 citedByCount "39" @default.
• W2922216511 countsByYear W29222165112019 @default.
• W2922216511 countsByYear W29222165112020 @default.
• W2922216511 countsByYear W29222165112021 @default.
• W2922216511 countsByYear W29222165112022 @default.
• W2922216511 countsByYear W29222165112023 @default.
• W2922216511 crossrefType "journal-article" @default.
• W2922216511 hasAuthorship W2922216511A5006674850 @default.
• W2922216511 hasAuthorship W2922216511A5009584320 @default.
• W2922216511 hasAuthorship W2922216511A5029123923 @default.
• W2922216511 hasAuthorship W2922216511A5069009768 @default.
• W2922216511 hasAuthorship W2922216511A5073938095 @default.
• W2922216511 hasAuthorship W2922216511A5087333416 @default.
• W2922216511 hasConcept C109007969 @default.
• W2922216511 hasConcept C111368507 @default.
• W2922216511 hasConcept C112959462 @default.
• W2922216511 hasConcept C114793014 @default.
• W2922216511 hasConcept C115880899 @default.
• W2922216511 hasConcept C126645576 @default.
• W2922216511 hasConcept C127313418 @default.
• W2922216511 hasConcept C151730666 @default.
• W2922216511 hasConcept C17409809 @default.
• W2922216511 hasConcept C187320778 @default.
• W2922216511 hasConcept C205649164 @default.
• W2922216511 hasConcept C2777844515 @default.
• W2922216511 hasConcept C2779429093 @default.
• W2922216511 hasConcept C2779870107 @default.
• W2922216511 hasConcept C2779899878 @default.
• W2922216511 hasConcept C2780049196 @default.
• W2922216511 hasConcept C2780789209 @default.
• W2922216511 hasConcept C2816523 @default.
• W2922216511 hasConcept C40212044 @default.
• W2922216511 hasConcept C40724407 @default.
• W2922216511 hasConcept C58640448 @default.
• W2922216511 hasConcept C76886044 @default.
• W2922216511 hasConceptScore W2922216511C109007969 @default.
• W2922216511 hasConceptScore W2922216511C111368507 @default.
• W2922216511 hasConceptScore W2922216511C112959462 @default.

• next