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- W2887447465 abstract "Identifying the geochemical characteristics of the surface fine-grained sediments in the mid-latitude deserts of Asia is essential for interpreting and tracing the aeolian sediments deposited in the far-away regions. The geochemical characteristics of ground surface fine-grained deposits (fractions < 63 μm in diameter) at five potential dust source areas (gobi deserts) of northwestern China, including the northern Qinghai-Tibet Plateau, the Tarim Basin, the Turpan-Hami Basin, the Hexi Corridor, and the Ala Shan Plateau, were investigated. The analytical results show that there are significant spatial differences in the geochemical characteristics among these regions. Geographically, the high contents of P, Ti, La, Ce, and Nd in the Tarim Basin, Mn, Co, Cu, Zn, Ga, Sr, Pb, and CaO in the Turpan-Hami Basin, Rb, Ba, Al2O3, Na2O, and K2O in the Hexi Corridor, and V, Cr, Ni, As, Y, Zr, Nb, SiO2, Fe2O3, and MgO in the Ala Shan Plateau, are identified. The spatial differences in the geochemical characteristics may be integrated signatures resulted from the differences in the fine-grained sediments’ formation, provenance, transportation, and deposition dynamics related to the local geologic and climatic settings. These mixed signatures in compositions may result in deviations in interpreting aeolian deposits far from the source regions, and consequently, affect their environmental implications as the proxies used in the past climate reconstructions." @default.
- W2887447465 created "2018-08-22" @default.
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- W2887447465 creator A5053385409 @default.
- W2887447465 creator A5057443470 @default.
- W2887447465 date "2018-10-01" @default.
- W2887447465 modified "2023-10-18" @default.
- W2887447465 title "Geochemical characteristics of the fine-grained component of surficial deposits from dust source areas in northwestern China" @default.
- W2887447465 cites W1968675387 @default.
- W2887447465 cites W1969576931 @default.
- W2887447465 cites W1970728125 @default.
- W2887447465 cites W1974270665 @default.
- W2887447465 cites W1974665052 @default.
- W2887447465 cites W1977912435 @default.
- W2887447465 cites W1980203794 @default.
- W2887447465 cites W1987023077 @default.
- W2887447465 cites W1987714605 @default.
- W2887447465 cites W1992378649 @default.
- W2887447465 cites W1992669909 @default.
- W2887447465 cites W1992796439 @default.
- W2887447465 cites W1997318182 @default.
- W2887447465 cites W1997350491 @default.
- W2887447465 cites W1997390689 @default.
- W2887447465 cites W1997453614 @default.
- W2887447465 cites W1997616766 @default.
- W2887447465 cites W1999011085 @default.
- W2887447465 cites W2000271298 @default.
- W2887447465 cites W2001361830 @default.
- W2887447465 cites W2003514269 @default.
- W2887447465 cites W2004024864 @default.
- W2887447465 cites W2005141551 @default.
- W2887447465 cites W2009221352 @default.
- W2887447465 cites W2015546718 @default.
- W2887447465 cites W2016116453 @default.
- W2887447465 cites W2018226281 @default.
- W2887447465 cites W2020706477 @default.
- W2887447465 cites W2027804120 @default.
- W2887447465 cites W2028260376 @default.
- W2887447465 cites W2028358324 @default.
- W2887447465 cites W2031593709 @default.
- W2887447465 cites W2034223887 @default.
- W2887447465 cites W2035585230 @default.
- W2887447465 cites W2036810320 @default.
- W2887447465 cites W2037703975 @default.
- W2887447465 cites W2038308820 @default.
- W2887447465 cites W2039166487 @default.
- W2887447465 cites W2040945899 @default.
- W2887447465 cites W2041781353 @default.
- W2887447465 cites W2046325330 @default.
- W2887447465 cites W2049441218 @default.
- W2887447465 cites W2051014865 @default.
- W2887447465 cites W2053300568 @default.
- W2887447465 cites W2055995241 @default.
- W2887447465 cites W2056358767 @default.
- W2887447465 cites W2056945332 @default.
- W2887447465 cites W2058350130 @default.
- W2887447465 cites W2059384657 @default.
- W2887447465 cites W2060706280 @default.
- W2887447465 cites W2060838133 @default.
- W2887447465 cites W2065918682 @default.
- W2887447465 cites W2072453480 @default.
- W2887447465 cites W2074904761 @default.
- W2887447465 cites W2081528020 @default.
- W2887447465 cites W2084378009 @default.
- W2887447465 cites W2088988148 @default.
- W2887447465 cites W2090245700 @default.
- W2887447465 cites W2090964269 @default.
- W2887447465 cites W2102526027 @default.
- W2887447465 cites W2105243677 @default.
- W2887447465 cites W2121165449 @default.
- W2887447465 cites W2123814711 @default.
- W2887447465 cites W2126178085 @default.
- W2887447465 cites W2154238011 @default.
- W2887447465 cites W2155699713 @default.
- W2887447465 cites W2158679230 @default.
- W2887447465 cites W2160811744 @default.
- W2887447465 cites W2171519564 @default.
- W2887447465 cites W2175723267 @default.
- W2887447465 cites W2184851138 @default.
- W2887447465 cites W2299684625 @default.
- W2887447465 cites W2488851807 @default.
- W2887447465 cites W2611293014 @default.
- W2887447465 cites W2625653296 @default.
- W2887447465 cites W2736893107 @default.
- W2887447465 cites W2749574947 @default.
- W2887447465 cites W4234728700 @default.
- W2887447465 doi "https://doi.org/10.1016/j.aeolia.2018.07.004" @default.
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