[1] Rao W B, Yang J D, Chen J, et al. Sr-Nd isotope geochemistry of eolian dust of the arid-semiarid areas in China: Implications for loess provenance and monsoon evolution[J]. Chinese Science Bulletin, 2006, 51(12): 1401-1412.
[2] Chen J, Li G J, Yang J D, et al. Nd and Sr isotopic characteristics of Chinese deserts: Implications for the provenances of Asian dust[J]. Geochimica et Cosmochimica Acta, 2007, 71(15): 3904-3914.
[3] Chen J, Li G J. Geochemical studies on the source region of Asian dust[J]. Science China Earth Sciences, 2011, 54(9): 1279-1301.
[4] Zhang X Y, Arimoto R, An Z S. Dust emission from Chinese desert sources linked to variations in atmospheric circulation[J]. Journal of Geophysical Research, 1997, 102(D23): 28041-28047.
[5] Sun J M. Source regions and formation of the loess sediments on the high mountain regions of northwestern China[J]. Quaternary Research, 2002, 58(3): 341-351.
[6] Sun J M. Provenance of loess material and formation of loess deposits on the Chinese Loess plateau[J]. Earth and Planetary Science Letters, 2002, 203(3/4): 845-859.
[7] Shi Z G, Liu X D. Distinguishing the provenance of fine-grained eolian dust over the Chinese Loess Plateau from a modelling perspective[J]. Tellus B: Chemical and Physical Meteorology, 2011, 63(5): 959-970.
[8] Che X D, Li G J. Binary sources of loess on the Chinese Loess Plateau revealed by U-Pb ages of zircon[J]. Quaternary Research, 2013, 80(3): 545-551.
[9] Chen Z, Li G J. Evolving sources of eolian detritus on the Chinese Loess Plateau since Early Miocene: Tectonic and climatic controls[J]. Earth and Planetary Science Letters, 2013, 371-372: 220-225.
[10] Nie J S, Peng W B, Möller A, et al. Provenance of the Upper Miocene-Pliocene Red Clay deposits of the Chinese loess plateau[J]. Earth and Planetary Science Letters, 2014, 407: 35-47.
[11] Nie J S, Peng W B. Automated SEM-EDS heavy mineral analysis reveals no provenance shift between glacial loess and interglacial paleosol on the Chinese Loess Plateau[J]. Aeolian Research, 2014, 13: 71-75.
[12] Zhang H Z, Lu H Y, Xu X S, et al. Quantitative estimation of the contribution of dust sources to Chinese Loess using detrital zircon U-Pb age patterns[J]. Journal of Geophysical Research, 2016, 121(11): 2085-2099.
[13] Grousset F E, Biscaye P E. Tracing dust sources and transport patterns using Sr, Nd and Pb isotopes[J]. Chemical Geology, 2005, 222(3/4): 149-167.
[14] Rao W B, Chen J, Yang J D, et al. Sr-Nd isotopic characteristics of eolian deposits in the Erdos Desert and Chinese Loess Plateau: Implications for their provenances[J]. Geochemical Journal, 2008, 42(3): 273-282.
[15] Li G J, Chen J, Ji J F, et al. Natural and anthropogenic sources of East Asian dust[J]. Geology, 2009, 37(8): 727-730.
[16] Li G J, Pettke T, Chen J. Increasing Nd isotopic ratio of Asian dust indicates progressive uplift of the north Tibetan Plateau since the middle Miocene[J]. Geology, 2011, 39(3): 199-202.
[17] 杨杰东,陈俊,饶文波,等. 中国沙漠的同位素分区特征[J]. 地球化学,2007,36(5):516-524.

Yang Jiedong, Chen Jun, Rao Wenbo, et al. Isotopic partition characteristics of Chinese deserts[J]. Geochimica, 2007, 36(5): 516-524.
[18] 裘善文. 中国东北西部沙地与沙漠化[M]. 北京:科学出版社,2008.

Qiu Shanwen. Sandy land and desertification in western Northeast China[M]. Beijing: Science Press, 2008.
[19] Wang Y X, Yang J D, Chen J, et al. The Sr and Nd isotopic variations of the Chinese Loess Plateau during the past 7 Ma: Implications for the East Asian winter monsoon and source areas of loess[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2007, 249(3/4): 351-361.
[20] 杨杰东,李高军,戴澐,等. 黄土高原黄土物源区的同位素证据[J]. 地学前缘,2009,16(6):195-206.

Yang Jiedong, Li Gaojun, Dai Yun, et al. Isotopic evidences for provenances of loess of the Chinese Loess Plateau[J]. Earth Science Frontiers, 2009, 16(6): 195-206.
[21] Yang J D, Li G J, Rao W B, et al. Isotopic evidences for provenance of East Asian Dust[J]. Atmospheric Environment, 2009, 43(29): 4481-4490.
[22] Rao W B, Mao C P, Wang Y G, et al. Using Nd-Sr isotopes and rare earth elements to study sediment provenance of the modern radial sand ridges in the southwestern Yellow Sea[J]. Applied Geochemistry, 2017, 81: 23-35.
[23] Bayon G, Toucanne S, Skonieczny C, et al. Rare earth elements and neodymium isotopes in world river sediments revisited[J]. Geochimica et Cosmochimica Acta, 2015, 170: 17-38.
[24] Smith J, Vance D, Kemp R A, et al. Isotopic constraints on the source of Argentinian loess-with implications for atmospheric circulation and the provenance of Antarctic dust during recent glacial maxima[J]. Earth and Planetary Science Letters, 2003, 212(1/2): 181-196.
[25] Feng J L, Zhu L P, Zhen X L, et al. Grain size effect on Sr and Nd isotopic compositions in eolian dust: Implications for tracing dust provenance and Nd model age[J]. Geochemical Journal, 2009, 43(2): 123-131.
[26] Li T G, Xu Z K, Lim D, et al. Sr-Nd isotopic constraints on detrital sediment provenance and paleoenvironmental change in the northern Okinawa Trough during the Late Quaternary[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2015, 430: 74-84.
[27] Derry L A, France-Lanord C. Neogene Himalayan weathering history and river 87Sr/86Sr: Impact on the marine Sr record[J]. Earth and Planetary Science Letters, 1996, 142(1/2): 59-74.
[28] Bi L, Yang S Y, Zhao Y, et al. Provenance study of the Holocene sediments in the Changjiang (Yangtze River) estuary and inner shelf of the East China Sea[J]. Quaternary International, 2017, 441: 147-161.
[29] 饶文波,杨杰东,陈骏,等. 北方风尘中Sr-Nd同位素组成变化的影响因素探讨[J]. 第四纪研究,2005,25(4):531-532.

Rao Wenbo, Yang Jiedong, Chen Jun, et al. Influences on Sr-Nd isotopic compositions in eolian dust,North China[J]. Quaternary Sciences, 2005, 25(4): 531-532.
[30] Dasch E J. Strontium isotopes in weathering profiles, deep-sea sediments, and sedimentary rocks[J]. Geochimica et Cosmochimica Acta, 1969, 33(12): 1521-1552.
[31] Meyer I, Davies G R, Stuut J B W. Grain size control on Sr-Nd isotope provenance studies and impact on paleoclimate reconstructions: An example from deep-sea sediments offshore NW Africa[J]. Geochemistry, Geophysics, Geosystems, 2011, 12(3): Q03005.
[32] Goldstein S L, O’Nions R K, Hamilton P J. A Sm-Nd isotopic study of atmospheric dusts and particulates from major river systems[J]. Earth and Planetary Science Letters, 1984, 70(2): 221-236.
[33] Nakai S, Halliday A N, Rea D R. Provenance of dust in the Pacific Ocean[J]. Earth and Planetary Science Letters, 1993, 119(1/2): 143-157.
[34] Dou Y G, Yang S Y, Shi X F, et al. Provenance weathering and erosion records in southern Okinawa Trough sediments since 28 ka: Geochemical and Sr-Nd-Pb isotopic evidences[J]. Chemical Geology, 2016, 425: 93-109.
[35] Yan Y, Sun Y B, Chen H Y, et al. Oxygen isotope signatures of quartz from major Asian dust sources: Implications for changes in the provenance of Chinese loess[J]. Geochimica et Cosmochimica Acta, 2014, 139: 399-410.
[36] Xie Y Y, Meng J, Guo L F. REE geochemistry of modern eolian dust deposits in Harbin city, Heilongjiang province, China: Implications for provenance[J]. CATENA, 2014, 123: 70-78.
[37] Qiang M, Lang L, Wang Z. Do fine-grained components of loess indicate westerlies: Insights from observations of dust storm deposits at Lenghu (Qaidam Basin, China)[J]. Journal of Arid Environments, 2010, 74(10): 1232-1239.
[38] Sun D H. Monsoon and westerly circulation changes recorded in the Late Cenozoic aeolian sequences of Northern China[J]. Global and Planetary Change, 2004, 41(1): 63-80.
[39] Sun D H, Bloemendal J, Rea D K, et al. Bimodal grain-size distribution of Chinese loess, and its palaeoclimatic implications[J]. CATENA, 2004, 55(3): 325-340.
[40] Roe G. On the interpretation of Chinese loess as a paleoclimate indicator[J]. Quaternary Research, 2009, 71(2): 150-161.
[41] Sun J M, Zhang M Y, Liu T S. Spatial and temporal characteristics of dust storms in China and its surrounding regions, 1960-1999: Relations to source area and climate[J]. Journal of Geophysical Research, 2001, 106(D10): 10325-10333.
[42] Ben-Israel M, Enzel Y, Amit R, et al. Provenance of the various grain-size fractions in the Negev loess and potential changes in major dust sources to the eastern Mediterranean[J]. Quaternary Research, 2015, 83(1): 105-115.
[43] Chen X L, Song Y G, Li J C, et al. Size-differentiated REE characteristics and environmental significance of aeolian sediments in the Ili Basin of Xinjiang, NW China[J]. Journal of Asian Earth Sciences, 2017, 143: 30-38.
[44] Prins M A, Vriend M. Glacial and interglacial eolian dust dispersal patterns across the Chinese Loess Plateau inferred from decomposed loess grain-size records[J]. Geochemistry, Geophysics, Geosystems, 2007, 8(7): Q07Q05.