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[1]XIAO Jingan,PEI Liang,SUN Liying,et al.Characteristics of Grain Sizes of Sediments in Two Typical Regions of Ejina Gobi[J].Research of Soil and Water Conservation,2021,28(03):38-44.
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Characteristics of Grain Sizes of Sediments in Two Typical Regions of Ejina Gobi

References:
[1] 冯益明,吴波,周娜,等.基于遥感影像识别的戈壁分类体系研究[J].中国沙漠,2013,33(3):635-641.
[2] Prospero J M, Ginoux P, Torres O, et al. Environmental Characterization of GLOBAL Sources of Atmospheric Soil DUST Identified with the NIMBUS 7 Total OZONE Mapping SPECTROMETER(toms)Absorbing Aerosol Product[J]. Rvgeo, 2002,40(1):1002, DOI:https:∥doi. org/10,1029/2000 RG000095.
[3] 赵松乔.中国干旱地区自然地理[M].科学出版社,1985.
[4] Owen L A, Windley B F, Cunningham W D, et al. Quaternary alluvial fans in the Gobi of southern Mongolia:Evidence for neotectonics and climate change[J]. Journal of Quaternary Ence, 2015,12(3):239-252.
[5] Hülle D, Hilgers A, Radtke U, et al. OSL dating of sediments from the Gobi Desert, Southern Mongolia[J]. Quaternary Geochronology, 2010,5(2/3):107-113.
[6] LüY W, Gu Z Y, Aldahan A, et al.10 Be in quartz gravel from the Gobi Desert and evolutionary history of alluvial sedimentation in the Ejina Basin, Inner Mongolia, China[J]. Chinese Science Bulletin, 2010,55(33):3802-3809.
[7] 任明达,王乃梁同.现代沉积环境概论[M].北京:科学出版社,1981.
[8] 孙东怀, Rea D.中国黄土粒度的双峰分布及其古气候意义[J].沉积学报,2000,18(3):327-335.
[9] 秦小光,吴金水,蔡炳贵,等.全新世时期北京—张家口地区与黄土高原地区风成系统的差异[J].第四纪研究,2004,24(4):430-436.
[10] 殷志强,秦小光,吴金水,等.湖泊沉积物粒度多组分特征及其成因机制研究[J].第四纪研究,2008,28(2):345-353.
[11] 刘富刚.鲁西北地表沉积物粒度特征及分布成因研究[J].人民黃河,2008,30(7):12-13.
[12] 殷志强,秦小光,吴金水,等.中国北方部分地区黄土,沙漠沙,湖泊,河流细粒沉积物粒度多组分分布特征研究[J].沉积学报,2009,27(2):343-351.
[13] 董智,王丽琴,杨文斌,等.额济纳盆地戈壁沉积物粒度特征分析[J].中国水土保持科学,2013,11(1):32-38.
[14] 肖晨曦,李志忠.粒度分析及其在沉积学中应用研究[J].新疆师范大学学报:自然科学版,2006,25(3):118-123.
[15] 钱广强,董治宝,罗万银,等.巴丹吉林沙漠地表沉积物粒度特征及区域差异[J].中国沙漠,2011,31(6):1357-1364.
[16] 魏豆豆,陈英玉.达连海湖泊沉积物粒度特征及其古气候意义[J].青海大学学报:自然科学版,2015,33(2):53-60.
[17] 毕志伟,杨振京,徐建明,等.塔里木盆地腹地第四纪沉积物粒度特征及其沉积环境[J].干旱区地理,2009,32(3):335-339.
[18] 王丽琴,李红丽,董智,等.额济纳盆地戈壁纵剖面沉积物粒度参数分析[J].水土保持研究,2014,21(1):152-156,162.
[19] Wünnemann B, Hartmann K, Janssen M, et al. Responses of Chinese desert lakes to climate instability during the past 45,000 years[J]. Developments in Quaternary Sciences, 2007,9:11-24.
[20] Zhang H C, Ming Q Z, Lei G L, et al. Dilemma of dating on lacustrine deposits in an hyperarid inland basin of NW China[J]. Radiocarbon, 2006,48(2):219-226.
[21] 迟振卿,王永,姚培毅,等.内蒙古额济纳旗地貌特征及其构造,气候事件[J].地质论评,2006,52(3):370-378.
[22] Krumbein W C. Measurement and geological significance of shape and roundness of sedimentary particles[J]. Journal of Sedimentary Research, 1941,11(2):64-72.
[23] 贾建军,高抒,薛允传.图解法与矩法沉积物粒度参数的对比[J].海洋与湖沼,2002,33(6):577-582.
[24] 徐树建,潘保田,张慧,等.末次冰期旋回风成沉积物图解法与矩值法粒度参数的对比[J].干旱区地理,2005,28(2):194-198.
[25] 毛龙江,庞奖励,刘晓燕.南京下蜀黄土图解法与矩值法粒度参数对比研究[J].陕西师范大学学报:自然科学版,2007,35(3):95-99.
[26] 徐兴永,易亮,于洪军,等.图解法和矩值法估计海岸带沉积物粒度参数的差异[J].海洋学报,2009,32(2):80-86.
[27] 刘志杰,龙海燕.南海沉积物图解法和矩值法粒度参数计算及对比[J].中国海洋大学学报:自然科学版,2009,39(2):313-316.
[28] 陶敏,邓山,王婷乐,等.矩值法和图解法计算山区河流沉积物粒度参数的差异[J].三峡大学学报:自然科学版,2012,33(6):27-32.
[29] 刘志杰,公衍芬,周松望,等.海洋沉积物粒度参数3种计算方法的对比研究[J].海洋学报,2013,35(3):179-188.
[30] McManus J. Grain size determination and interpretation[R]. Techniques, in Sedimentology, 1988.
[31] Blott S J, Pye K. GRADISTAT:a grain size distribution and statistics package for the analysis of unconsolidated sediments[J]. Earth Surface Processes & Landforms, 2010,26(11):1237-1248.
[32] 屈建军,黄宁,拓万全,等.戈壁风沙流结构特性及其意义[J].地球科学进展,2005,20(1):19-23.
[33] 雷国良.额济纳盆地晚更新世以来湖相沉积记录与环境演变[D].兰州:兰州大学,2009.
[34] 王飞燕,王富葆,王雪瑜.地貌学与第四纪地质学[M].北京:高等教育出版社,1990.
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