Blatt H, Middleton G, Murray R, 1980. Origin of Sedimentary Rocks. Prentice-Hall, Inc.
Chen G Y, Dai X R, Zhang M J, 1995. Study on the heavy minerals in the dustfall of the severe duststorm numbered 930505 in Lanzhou area, Gansu Province. Journal of Desert Research, 15(4): 374-377. (in Chinese)
Chen J, An Z S, Liu L W et al., 2001. Variations in chemical compositions of the eolian dust in Chinese Loess Plateau over the past 2.5Ma and chemical weathering in the Asian inland. Science in China (Series D), 31(2): 136-145.
Chen J, Ji J F, Chou G et al., 1997. Geochemistry of the chemical weathering intensity of the loess profile in Luochuan, Shaanxi Province. Science in China (Series D), 27(6):531-536.
Chen J, Li G J, Yang J D et al., 2007. Nd and Sr isotopic characteristics of Chinese deserts: Implications for the provenances of Asian dust. Geochimica et Cosmochimica Acta, 71(15): 3904-3914.
Chen Y, Chen J, Liu L W, 2001. Chemical composition and characterization of chemical weathering of late Tertiary red clay in Xifeng, Gansu Province. Journal of Geomechanics, 7(2): 167-175. (in Chinese)
Ding Z L, Sun J M, Yang S L et al., 2001. Geochemistry of the Pliocene red clay formation in the Chinese Loess Plateau and implications for its origin, source provenance and paleoclimate change. Geochimica et Cosmochimica Acta, 65(6): 901-913.
Dong Z B, Qu J J, Wang X M et al., 2008. Pseudo-feathery dunes in the Kumtagh Desert. Geomorphology, 100(3/4): 328-334.
E Y H, Su Z Z, Wang J H et al., 2006. Outcome and scientific significance of integrated investigation in Kumtag Desert. Journal of Desert Research, 26(5): 693-697. (in Chinese)
E Y H, Wang J H, Yan P et al., 2008. Evolution of palaeo-drainage system and its relationship with the formation of desert landform in the Kumtag Desert. Acta Geographica Sinica, 63(7): 725-734. (in Chinese)
He Q, Yang X H, Huo W et al., 2009. Characteristics of sand granularity from Kumtag Desert and its environmental significance. Journal of Desert Research, 29(1): 18-22. (in Chinese)
Jickells T D, An Z S, Andersen K K et al., 2005. Global iron connections between desert dust, ocean biogeochemistry, and climate. Science, 308: 67-71.
Johnsson M J, Stallard R F, Lundberg N, 1991. Controls on the composition of fluvial sands from a tropical weathering environment: Sands of the Orinoco River drainage basin, Venezuela and Colombia. Geological Society of America Bulletin, 103(12): 1622-1647.
Johnsson M J, Stallard R F, Meade R H, 1988. First-cycle quartz arenites in the Orinoco River Basin, Venezuela and Colombia. Journal of Geology, 96: 263-277.
Li X S, Han Z Y, Chen Y Y et al., 2009. Characteristics and source of rain dust in Nanjing on March 11, 2006. Quaternary Sciences, 29(1): 43-54. (in Chinese)
Li X S, Han Z Y, Yang S Y et al., 2007. Chemical weathering intensity and element migration features of the Xiashu Loess profile in Zhenjiang. Acta Geographica Sinica, 62(11): 1174-1184. (in Chinese)
Lu H Y, Wang X Y, Li L P, 2010. Aeolian sediment evidence that global cooling has driven late Cenozoic stepwise aridification in central Asia. In: Clift P D, Tada R, Zheng H (eds.). Monsoon Evolution and Tectonics-Climate Linkage in Asia. Geological Society, London, Special Publications, 342: 29-44.
Muhs D, 2004. Mineralogical maturity in dunefields of North America, Africa and Australia. Geomorphology, 59(1-4): 247-269.
Nesbitt H, Markovics G, 1997. Weathering of granodioritic crust, long-term storage of elements in weathering profiles, and petrogenesis of siliciclastic sediments. Geochimica et Cosmochimica Acta, 61(8): 1653-1670.
Nesbitt H, Young G, 1996. Petrogenesis of sediments in the absence of chemical weathering: effects of abrasion and sorting on bulk composition and mineralogy. Sedimentology, 43(2): 341-358.
Nesbitt H W, Young G M, 1982. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature, 299(21): 715-717.
Ohta T, Arai H, 2007. Statistical empirical index of chemical weathering in igneous rocks: A new tool for evaluating the degree of weathering. Chemical Geology, 240(3/4): 280-297.
Qian Y B, Wu Z N, Ishii T et al., 1993. The constituent characteristics of sand materials and sand sources of Taklamakan Desert. Journal of Desert Research, 13(4): 32-38. (in Chinese)
Qian Y B, Zhou X J, Li C S et al., 2001. Multi-sources of sand minerals for the deserts in the Jungger Basin. Journal of Desert Research, 21(2): 182-187. (in Chinese)
Qu J J, Liao K T, Zu R P et al., 2007. Study on formation mechanism of feather-shaped sand ridge in Kumtag Desert. Journal of Desert Research, 27(3): 349-354. (in Chinese)
Qu J J, Zuo G C, Zhang K C et al., 2005. Relationship between the formation and evolution of the Kumtag Desert and the regional Neotectonic movement. Arid Land Geography, 28(4): 424-428. (in Chinese)
Ritts B D, Biffi U, 2000. Magnitude of post-Middle Jurassic displacement on the central Altyn Tagh fault system, Northwest China. Geological Society of American Bulletin, 112(1): 61-74.
Shi Y X, Dai X R, Li J T et al., 1995. On the wind-blown deposits from a heavy dust fall numbered “930505” in Lanzhou, North-Central China. Acta Sedimentologica Sinica, 13(3): 76-82. (in Chinese)
Stevens T, Palk C, Carter A et al., 2010. Assessing the provenance of loess and desert sediments in northern China using U-Pb dating and morphology of detrital zircons. Geological Society of America Bulletin, 122: 1331-1344.
Sun J M, Li Y, Zhang Z Q et al., 2009. Magnetostratigraphic data on the Neogene growth folding in the foreland basin of the southern Tianshan Mountains. Geology, 37, 1051-1054.
Sun J M, Liu T S, 2006. The age of the Taklimakan Desert. Science, 312: 1621.
Taylor S R, McLennan S M, 1985. The Continental Crust: Its Composition and Evolution. London: Blackwell, 277.
Turekian K K, Wedepohl K H, 1961. Distribution of the elements in major units of the earth crust. Bulletin of the Geological Society of America, 72(2): 175-192.
Újvári G, Varga A, Balogh-Brunstad Z, 2008. Origin, weathering, and geochemical composition of loess in southwestern Hungary. Quaternary Research, 69(3): 421-437.
Wang S J, 1987. Formation of Aqik valley in the east of Lop Nor. Lop Nor Comprehensive Scientific Expedition Team, Xinjiang Branch of Chinese Academy of Sciences, Lop Nor Scientific Expedition and Research. Beijing: Science Press, 60-67. (in Chinese)
Weltje G J, von Eynatten H, 2004. Quantitative provenance analysis of sediments: Review and outlook. Sedimentary Geology, 171(1-4): 1-11.
Xia X C, 1987. Basic character of Kumtag Desert. Lop Nor Comprehensive Scientific Expedition Team, Xinjiang Branch of Chinese Academy of Sciences, Lop Nor Scientific Expedition and Research. Beijing: Science Press, 52-59, 78-94. (in Chinese)
Xie J, Ding Z L, 2007. Compositions of heavy minerals in Northeastern China sandlands and provenance analysis. Science in China (Series D), 50(11): 1715-1723.
Xie Y Y, He K, Zhou J et al., 2006. Chemical characteristic of dust storm deposits in Harbin and its matter origin. Geographical Research, 25(2): 255-261. (in Chinese)
Yang X B, Zhu B Q, White P D, 2007. Provenance of aeolian sediment in the Taklamakan Desert of western China, inferred from REE and major-elemental data. Quaternary International, 175(1): 71-85.
Young G, Nesbitt H, 1998. Processes controlling the distribution of Ti and Al in weathering profiles, siliciclastic sediments and sedimentary rocks. Journal of Sedimentary Research, 68(3): 448-455.
Zhang S, Liu P, Jin C S et al., 2008. Geochemistry of the heavy dust fall on 17 April 2006 in Beijing. Marine Geology & Quaternary Geology, 28(3): 36-42. (in Chinese)
Zhang X Y, Wang Y Q, Wang D et al. Characterization and sources of regional-scale transported carbonaceous and dust aerosols from different pathways in coastal and sandy land areas of China. Journal of Geophysical Research, 2005, 110(D15): D15301.
Zhang Z Q, Sun J M, 2011. Palynological evidence for Neogene environmental change in the foreland basin of the southern Tianshan range, northwestern China. Global and Planetary Change, 75, 56-66.
Zheng H, Powell C, An Z et al., 2000. Pliocene uplift of the northern Tibetan Plateau. Geology, 28(8): 715-718. |