[1]WANG Li-qin,LI Hong-li,DONG Zhi,et al.Particle Size Characteristics of Sediment Profile in Gobi of Ejina Basin[J].Research of Soil and Water Conservation,2014,21(01):152-156,162.
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Particle Size Characteristics of Sediment Profile in Gobi of Ejina Basin

References:
[1] 王贵勇,董光荣,李森,等.试论戈壁面及指相意义[J].中国沙漠,1995,15(2):124-130.
[2] 吴正.风沙地貌学[M].北京:科学出版社,1987.
[3] 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.
[4] 任明达,王乃梁.现代沉积环境概论[M].北京:科学出版社,1981:8-93.
[5] 刘富刚.鲁西北地表沉积物粒度特征及分布成因研究[J].人民黄河,2008,30(7):12-13,29.
[6] 蒋庆丰,刘兴起,沈吉,等.乌伦古湖沉积物粒度特征及其古气候环境意义[J].沉积学报,2006,24(6):879-881.
[7] 董玉祥.海岸现代风成砂粒度参数特征的研究:以中国温带海岸为例[J].沉积学报,2002,20(4):656-662.
[8] 曹振,胡克,张永光,等.科尔沁沙地地表沉积物粒度分析与可风蚀性讨论[J].中国沙漠,2005,25(1):15-19.
[9] 李柏,高甲荣,胡封兵,等.北京王虎沟泥石流堆积物粒度参数分析[J].中国水土保持学报,2011,9(4):7-10.
[10] 谢柯.内蒙古额济纳旗松散沉积物的粒度分异特征及其沉积环境[D].长沙:湖南师范大学,2008.
[11] 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.
[12] 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.
[13] 战庆,王张华,王昕,等.长江口区晚新生代沉积物粒度特征和沉积地貌环境演变[J].沉积学报,2009,27(4):675-681.
[14] 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.
[15] Folk R L, Ward W C.Brazos river bar:A study in significance of grain size parameters[J].Journal of Sedimentary Petrology,1957,27(1):3-24.
[16] Krumbein W C. Measurement and geological significance of shape and roundness of sedimentary particles[J].Jour. Sed. Petrology, 1941,11(2):64-72.
[17] 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,1990:5-61.
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