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• W2289366704 endingPage "61" @default.
• W2289366704 startingPage "43" @default.
• W2289366704 abstract "A strong dust-storm event occurred in Harbin, China on May 11, 2011. The dry- and wet-deposited dust depositions in this dust-storm event, together with the surface sediments from the potential sources, were collected to study grain size distributions, carbonate content and carbon isotopic composition of carbonate, major element, trace element and rare earth elements (REE), and Sr–Nd isotopic compositions. The results indicate as follows. The dry-deposited dusts are characterized by bimodal grain-size distributions with a fine mode at 3.6 μm and a coarse mode at 28 μm whereas the wet-deposited dusts are indicative of unimodal grain-size modes with a fine mode at 6 μm. The dust-storm depositions are influenced to a certain extent by sedimentary sorting and are of a derivation from the recycled sediments. Based on identifying the immobility of element pairs before constraining sources of dust-storm deposits using geochemical elements, in conjunction with REE and especially Sr–Nd isotopic compositions, the primary and strengthening sources for the dust-storm event were detected, respectively. The Hunsandake Sandy Land as the primary source and the Horqin Sandy Land as the strengthening source were together responsible for the derivation of dust depositions during dust-storm event. The Hunsandake Sandy Land, however, contributes less dust to the dust-storm event in Harbin compared to the Horqin Sandy Land, and the Hulun Buir Sandy Land is undoubtedly excluded from being one of the sources for dust-storm depositions in Harbin. There are not notable differences in geochemical (especially Sr–Nd isotopic) compositions between dry- and wet-deposited dusts, indicating that the wet-deposited dust is of identical derivation to the dry-deposited dust. Based on our observations, it is of interest to suggest that fine and coarse particles in the CLP (Chinese Loess Plateau) loess possibly have the same sources." @default.
• W2289366704 created "2016-06-24" @default.
• W2289366704 creator A5030042849 @default.
• W2289366704 creator A5049625251 @default.
• W2289366704 date "2016-04-01" @default.
• W2289366704 modified "2023-10-14" @default.
• W2289366704 title "Geochemical investigation of dry- and wet-deposited dust during the same dust-storm event in Harbin, China: Constraint on provenance and implications for formation of aeolian loess" @default.
• W2289366704 cites W1964883926 @default.
• W2289366704 cites W1965351011 @default.
• W2289366704 cites W1965536973 @default.
• W2289366704 cites W1968346323 @default.
• W2289366704 cites W1968437447 @default.
• W2289366704 cites W1969576931 @default.
• W2289366704 cites W1972481325 @default.
• W2289366704 cites W1974270665 @default.
• W2289366704 cites W1975042776 @default.
• W2289366704 cites W1976170009 @default.
• W2289366704 cites W1976519522 @default.
• W2289366704 cites W1977880023 @default.
• W2289366704 cites W1979562936 @default.
• W2289366704 cites W1982291435 @default.
• W2289366704 cites W1983175453 @default.
• W2289366704 cites W1983246059 @default.
• W2289366704 cites W1983409145 @default.
• W2289366704 cites W1988627424 @default.
• W2289366704 cites W1992814246 @default.
• W2289366704 cites W1994233909 @default.
• W2289366704 cites W1995373137 @default.
• W2289366704 cites W1997921102 @default.
• W2289366704 cites W2000847860 @default.
• W2289366704 cites W2001800904 @default.
• W2289366704 cites W2009979849 @default.
• W2289366704 cites W2010086345 @default.
• W2289366704 cites W2010925982 @default.
• W2289366704 cites W2013158150 @default.
• W2289366704 cites W2013326080 @default.
• W2289366704 cites W2015876559 @default.
• W2289366704 cites W2016109297 @default.
• W2289366704 cites W2016536555 @default.
• W2289366704 cites W2016848487 @default.
• W2289366704 cites W2016924367 @default.
• W2289366704 cites W2018790242 @default.
• W2289366704 cites W2019874086 @default.
• W2289366704 cites W2021300589 @default.
• W2289366704 cites W2024462323 @default.
• W2289366704 cites W2025069593 @default.
• W2289366704 cites W2029276637 @default.
• W2289366704 cites W2029715822 @default.
• W2289366704 cites W2032089883 @default.
• W2289366704 cites W2033569711 @default.
• W2289366704 cites W2034636860 @default.
• W2289366704 cites W2035585230 @default.
• W2289366704 cites W2038902323 @default.
• W2289366704 cites W2038908563 @default.
• W2289366704 cites W2041230190 @default.
• W2289366704 cites W2042324412 @default.
• W2289366704 cites W2044952811 @default.
• W2289366704 cites W2049581925 @default.
• W2289366704 cites W2050716036 @default.
• W2289366704 cites W2056139142 @default.
• W2289366704 cites W2057228997 @default.
• W2289366704 cites W2057389871 @default.
• W2289366704 cites W2059740507 @default.
• W2289366704 cites W2059835945 @default.
• W2289366704 cites W2069029376 @default.
• W2289366704 cites W2069641347 @default.
• W2289366704 cites W2077988709 @default.
• W2289366704 cites W2078140135 @default.
• W2289366704 cites W2083290992 @default.
• W2289366704 cites W2084378009 @default.
• W2289366704 cites W2085228574 @default.
• W2289366704 cites W2087705681 @default.
• W2289366704 cites W2087937118 @default.
• W2289366704 cites W2091008893 @default.
• W2289366704 cites W2092677927 @default.
• W2289366704 cites W2095557497 @default.
• W2289366704 cites W2097763036 @default.
• W2289366704 cites W2102832616 @default.
• W2289366704 cites W2111590126 @default.
• W2289366704 cites W2118364502 @default.
• W2289366704 cites W2121165449 @default.
• W2289366704 cites W2122766310 @default.
• W2289366704 cites W2123814711 @default.
• W2289366704 cites W2124460270 @default.
• W2289366704 cites W2127650736 @default.
• W2289366704 cites W2128981389 @default.
• W2289366704 cites W2134304039 @default.
• W2289366704 cites W2147127632 @default.
• W2289366704 cites W2152256665 @default.
• W2289366704 cites W2162898351 @default.
• W2289366704 cites W2164915920 @default.
• W2289366704 cites W2184851138 @default.
• W2289366704 cites W2247098479 @default.
• W2289366704 cites W2318880822 @default.
• W2289366704 cites W2563452930 @default.
• W2289366704 doi "https://doi.org/10.1016/j.jseaes.2016.01.025" @default.
• W2289366704 hasPublicationYear "2016" @default.
• W2289366704 type Work @default.

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