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    哈尔滨黄山黄土粒度特征及其对成因的指示

    魏传义 李长安 康春国 常国瑞

    魏传义, 李长安, 康春国, 常国瑞, 2015. 哈尔滨黄山黄土粒度特征及其对成因的指示. 地球科学, 40(12): 1945-1954. doi: 10.3799/dqkx.2015.175
    引用本文: 魏传义, 李长安, 康春国, 常国瑞, 2015. 哈尔滨黄山黄土粒度特征及其对成因的指示. 地球科学, 40(12): 1945-1954. doi: 10.3799/dqkx.2015.175
    Wei Chuanyi, Li Chang'an, Kang Chunguo, Chang Guorui, 2015. Grain-Size Characteristics and Genesis of the Huangshan Loess in Songnen Plain Area. Earth Science, 40(12): 1945-1954. doi: 10.3799/dqkx.2015.175
    Citation: Wei Chuanyi, Li Chang'an, Kang Chunguo, Chang Guorui, 2015. Grain-Size Characteristics and Genesis of the Huangshan Loess in Songnen Plain Area. Earth Science, 40(12): 1945-1954. doi: 10.3799/dqkx.2015.175

    哈尔滨黄山黄土粒度特征及其对成因的指示

    doi: 10.3799/dqkx.2015.175
    基金项目: 

    国家自然科学基金项目 41440002

    详细信息
      作者简介:

      魏传义(1990-),男,硕士,主要从事第四纪沉积与环境变化研究.E-mail: weichuanyi@126.com

      通讯作者:

      李长安,E-mail: chanli@cug.edu.cn

    • 中图分类号: P534.63

    Grain-Size Characteristics and Genesis of the Huangshan Loess in Songnen Plain Area

    • 摘要: 哈尔滨黄山黄土是东北地区黄土沉积的典型代表,其成因研究是恢复东北地区古气候和古环境的基础.为探讨松嫩平原地区中更新世晚期黄土成因问题,对具代表性的哈尔滨黄山黄土剖面进行系统、高分辨率的粒度和磁化率特征分析,并与哈尔滨现代沙尘沉降物、黄土高原典型黄土-古土壤、现代河流沉积物及大连市滨海黄土粒度特征进行对比.结果显示:黄山黄土粉砂级(10~50 μm)颗粒和黏土颗粒(<5 μm)的平均含量分别是43.86%(主众数粒组)和23.40%(次众数粒组);各粒度参数的平均值为:分选系数标准偏差σ=1.83、平均粒径Mz=6.25φ、中值粒径Md=5.89φ、偏度SK=0.21、峰态KG=0.86、中值粒径Kd=2.01;粒度频率曲线以双峰态分布为主,且主峰突出;岩性三角投影图、粒度象(C-M图、L-M图、A-M图)投影图及粒度参数(Mz-σMz-SKMz-KG)散点投影图与风成沉积物基本一致,但与河流沉积物差异明显;判别函数Y<0.基于以上粒度特征分析表明哈尔滨黄山黄土为典型的风成成因.

       

    • 图  1  采样剖面及研究区概况

      Fig.  1.  The overview of research area and sampling locations

      图  2  黄山剖面哈尔滨黄土岩性柱和中值粒径、体积磁化率变化曲线

      Fig.  2.  Lithological column, median diameter and magnetic susceptibility curve of Huangshan Loess

      图  3  哈尔滨黄山黄土岩性三角图

      Shepard(1954)Link(1966)

      Fig.  3.  Clay-silt-sand triangular plots of "Huangshan Loess" in Harbin area

      图  4  不同类型沉积物粒度频率曲线分布

      a.哈尔滨黄山古土壤;b.哈尔滨黄山黄土;c.松花江哈尔滨段河流沉积物(据何葵等, 2008);d.哈尔滨现代沙尘沉降物(据何葵等, 2009)

      Fig.  4.  Grain size frequency distribution curves of different sediments

      图  5  哈尔滨黄山黄土与河流沉积物粒度象对比

      a.C-M图;b.L-M图;c.A-M图;C值为百分之一含量的粒度;L值为<30 μm组分的重量百分数;A值为<4 μm组分的重量百分数;●表示本文"黄山黄土";A.现代河流沉积物粒度象投影区域;B.风成黄土粒度象投影区域(据李长安等(2010)修改)

      Fig.  5.  Comparison of grain size images of Huangshan Loess and fluvial sediment

      图  6  "哈尔滨黄山黄土"及河流沉积物粒度参数散点

      ●表示本文"黄山黄土";A.现代河流沉积物参数散点投影区域;B.为风成黄土参数散点投影区域(据李长安等(2010)修改)

      Fig.  6.  Comparison of scatter diagram of Huangshan Loess and fluvial sediment

      图  7  哈尔滨黄山黄土判别函数值

      Fig.  7.  Y value of grain size distribution of Huangshan Loess

      表  1  黄山黄土粒度组成与不同类型沉积物的对比

      Table  1.   Comparison of grain size composition between Huangshan Loess and different sediments

      采样地点 度量属性 粒级(%) 来源文献
      >50 μm 10~50 μm 5~10 μm <5 μm
      哈尔滨黄山黄土 全样最大值 57.22 51.15 19.96 31.41 本文数据
      全样最小值 10.03 31.60 3.78 4.75
      全样平均值 18.51 43.94 14.64 22.91
      哈尔滨黄山古土壤 全样最大值 44.91 52.38 20.97 32.98 本文数据
      全样最小值 8.35 31.35 4.27 5.34
      全样平均值 15.88 43.72 16.15 24.26
      哈尔滨现代沙尘沉降物 全样最大值 21.70 52.00 49.46 22.19 谢远云等(2005)何葵等(2009)
      全样最小值 2.89 25.44 19.20 7.10
      全样平均值 9.04 36.29 36.93 17.67
      现代河流沉降物 全样最大值 91.60 45.40 17.70 7.00 李长安等(2010)
      全样最小值 30.80 2.30 2.30 0.00
      全样平均值 77.40 15.80 5.00 1.80
      大连市七顶山黄土 全样最大值 59.17 79.76 2.44 吕金福和李志民(1990)张威等(2008)刘庆宏和贾亮(2010)
      全样最小值 17.61 49.06 0.17
      全样平均值 31.91 66.94 1.15
      洛川剖面(离石上部) 黄土 10.00 52.70 11.00 26.30 刘东生等(1985)
      古土壤 7.10 45.70 12.70 32.00
      下载: 导出CSV

      表  2  黄山黄土与不同类型沉积物粒度参数的对比

      Table  2.   Comparison of grain size measured between Huangshan loess and different sediments

      采样地点 度量属性 粒度参数 来源文献
      Md(φ) Mz(φ) σ SK KG Kd
      哈尔滨黄山黄土 全样最大值 6.68 6.67 2.05 0.49 1.53 8.51 本文数据
      全样最小值 4.11 4.47 1.16 -0.04 0.75 1.11
      全样平均值 5.89 6.25 1.83 0.21 0.86 2.01
      哈尔滨现代风尘沉降物 全样最大值 28.40 2.08 0.18 1.49 7.30 谢远云等(2005)何葵等(2009)
      全样最小值 8.44 1.50 -0.02 1.04 1.15
      全样平均值 13.87 1.78 0.09 1.17 2.64
      下蜀黄土 全样最大值 7.23 1.86 0.83 2.71 李徐生等(2001)
      全样最小值 6.27 1.38 0.36 1.29
      全样平均值 6.65 1.75 0.52 1.76
      大连市七顶山黄土 全样最大值 5.72 5.20 2.21 0.41 1.14 吕金福和李志民(1990)张威等(2008)刘庆宏和贾亮(2010)
      全样最小值 2.83 3.44 1.61 -0.39 0.69
      全样平均值 4.81 4.56 1.90 -0.16 0.81
      注:表中Md为中值粒径;Mz为平均粒径;σ为分选系数(标准偏差);SK为偏度;KG为峰态;Kd值=粗粉砂(10~50 μm)/黏粒(<5 μm).
      下载: 导出CSV
    • Pavlin Andrianof, B.H., Yu, P.L., Shi, S.M., et al., 1956. Genesis of Loess in China. Chinese Science Bulletin, 11: 1-15(in Chinese).
      Cai, M.T., Wei, M.J., 2009. Climate Change during the Penultimate Interglacial in Luochuan Area. Journal of Desert Research, 29(3): 536-543(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZGSS200903027.htm
      Cao, Z., Zhu, X.D., 2014. Research on the Formation Reason of Loess in Middle and Eastern Place in Northeast China. Journal of Changchun Normal University: Natural Science, (2): 85-89(in Chinese with English abstract). doi: 10.3969/j.issn.1008-178X.2014.02.024
      Chu, B.J., Gao, Z.C., Yang, S.S., et al., 1988. Quaternary Magnetostratigraphic Classification of the Song-Nen Plain (Songhuajiang River-Nenjiang River Plain). Marine Geology & Quaternary Geology, 8(4): 91-96 (in Chinese with English abstract). http://cat.inist.fr/?amodele=affichen&cpsidt=7215189
      Folk, R.L., Ward, W.C., 1957. Brazos River Bar: A Study in the Signification of Grain Size Parameters. Journal of Sedimentary Petrology, 27: 3-27. doi: 10.1306/74D70646-2B21-11D7-8648000102C1865D
      He, K., Kuang, C.G., Zhang, L.J., 2008. Relation between Riverbed Alluvial Deposits in the Harbin Reach of the Songhuajiang River and Sand-Dust Weather. Geology in China, 35(1): 150-156(in Chinese with English abstract). doi: 10.3969/j.issn.1000-3657.2008.01.016
      He, K., Xie, Y.Y., Kang, C.G., et al., 2009. Grain-Size Distributions of Harbin Fallouts and Its Source Areas. Chinese Agricultural Science Bulletin, 25(11): 200-205(in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_chinese-agricultural-science-bulletin_thesis/020126373183.html
      He, K., Xie, Y.Y., Zhang, L.J., et al., 2005. Grain Size Characteristic of Sand-Dust Sedimentary in Harbin City and Its Implication. Scientia Geographica Sinica, 25(5): 597-600(in Chinese with English abstract). doi: 10.3969/j.issn.1000-0690.2005.05.014
      Hu, B.R., Lu, Y.C., 1989. The "Silt to Clay" Ratio, Kd, and the Grain-Size Cycles of a Loess Section at Luochuan, Shanxi Province. Acta Petrologica Sinica, 5(1): 12-20 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB198901001.htm
      Kang, C.G., Li, C.A., Xie Y.Y., et al., 2011. Heavy Mineral Characteristics of Eolian Loess Deposits in Harbin Area and Its Provenance Implications. Journal of Natural Disasters, 20(4): 43-51 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZRZH201104006.htm
      Li, C.A., Zhang, Y.F., Yuan, S.Y., et al., 2010. Grain Size Characteristics and Origin of the "Wushan Loess" at Wushan Area. Earth Science—Journal of China University of Geosciences, 35(5): 879-884(in Chinese with English abstract). doi: 10.3799/dqkx.2010.102
      Li, C.Y., Wang, Z.T., Lin, S.Z., et al., 2004. The Relationship between East Asian Summer Monsoon Activity and Northward Jump of the Upper Westerly Jet Location. Chinese Journal of Atmospheric Sciences, 28(5): 641-658(in Chinese with English abstract). http://www.oalib.com/paper/1556788
      Li, L., 2009. Paleo-Environmental Information Study of Sea Shore Loess in Dalian (Dissertation). Liaoning Normal University, Liaoning, 1-51(in Chinese with English abstract).
      Li, X.M., 2001. Sedimentary Characteristics of Seashore Loess in South Liaoning. Marine Sciences, 25(1): 32-35(in Chinese with English abstract). doi: 10.3969/j.issn.1000-3096.2001.01.012
      Li, X.S., Yang, D.Y., Lu, H.Y., 2001. Grain-Size Features and Genesis of the Xiashu Loess in Zhenjiang. Marine Geology & Quaternary Geology, 21(1): 25-32(in Chinese with English abstract).
      Liu, D.S., An, Z.S., Zheng, H.H., 1985. Loess and Environment. Science Press, Beijing, 191-379(in Chinese).
      Liu, D.S., Ding, Z.L., Guo, Z.T., et al., 1991. Loess, and Arid Environment. Anhui Science and Technology Publishing House, Anhui, 34-278(in Chinese).
      Liu, Q.H., Jia, L., 2010. Analysis of Loess Sedimentary Characteristics in Dalian Costal Qidingshan. Journal of Liaoning Teachers College, 2: 50-51, 89(in Chinese).
      Liu, X.M., Liu, D.S., Xia, D.S., et al., 2007b. Analysis on Two Models of Paleoclimatic Records of Magnetic Susceptibility under Redox Conditions of Siberia and Chinese Loess. Science in China(Series D), 37(10): 1382-1391(in Chinese with English abstract).
      Liu, X.M., Xia, D.S., Liu, D.S., et al., 2007a. Discussion on Two Models of Paleoclimatic Records of Magnetic Susceptibility of Alaskan and Chinese Loess. Quaternary Sciences, 27(2): 210-220(in Chinese with English abstract). http://www.researchgate.net/publication/284515845_Discussion_on_two_models_of_paleoclimatic_records_of_magnetic_susceptibility_of_Alaskan_and_Chinese_loess
      Link, A.G., 1966. Textural Classification of Sediments. Sedimentology, 7(3): 249-254. doi: 10.1111/j.1365-3091.1966.tb01598.x
      Lu, H.Y., An, Z.S., 1998. Paleoclimatic Significance of Grain Size of Loess-Palaeosol Deposit in Chinese Loess Plateau. Science in China (Series D), 41(6): 626-631. doi: 10.1007/bf02878745
      Lu, H.Y., An, Z.S., 1999. Comparison of grain-size distribution of Red Clay and Loess-paleosol deposits in Chinese Loess Plateau. Acta Sedimentological Sinica, 2: 61-67(in Chinese with English abstract). http://www.researchgate.net/publication/281333487_Comparison_of_grain-size_distribution_of_red_clay_and_loess-paleosol_deposits_in_Chinese_Loess_Plateau
      Lü, J.F., Li, Z.M., 1990. Loess and its Sedimentary Environment in Liaodong Peninsula. Scientia Geographica Sinica, 10(2): 97-106, 191 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DLKX199002000.htm
      Pye, K., 1987. Aeolian Dust and Dust Deposits. Academic Press, Pittsburgh, 127-238. http://www.sciencedirect.com/science/book/9780125686907
      Ren, J.Z., Quan, H., Ding, Z.L., et al., 1997. An Example of the Second Last Glacial Period of Rapid Climate Change: Climate Instability Record in Huining Loess. Chinese Science Bulletin, 17: 1836-1839(in Chinese).
      Ren, S.F., Zheng, X.M., Ai, D.S., et al., 2014. Influence of Pretreatmene Methods on Grain-Size Distribution Pattern of the Xiashu Loess. Marine Geology and Quaternary Geology, (3): 185-194(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-HYDZ201403027.htm
      Shepard, F.P., 1954. Nomenclature Based on Sand-Silt-Clay Ratios. Journal of Sedimentary Research, 24: 151-158. http://ci.nii.ac.jp/naid/30003288053
      Sun, D.H., Lu, H.Y., 2007. Grain-Size and Dust Accumulation Rate of Late Cenozoic Aeolian Deposits and the Inferred Atmospheric Circulation Evolutions. Quaternary Sciences, 27(2): 251-262(in Chinese with English abstract). http://www.researchgate.net/publication/288261598_Grain-size_and_dust_accumulation_rate_of_late_Cenozoic_Aeolian_deposits_and_the_inferred_atmospheric_circulation_evolutions
      Sun, D.H., Lu, H.Y., David R., et al., 2000. Bimode Grain-Size Distribution of Chinese Loess and Its Paleoclimate Implication. Acta Sedimentologica Sinica, 18(3): 327-335 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB200003000.htm
      Sun, D.H., Shaw, J., An, Z.S., et al., 1998. Magnetostratigraphy and Paleoclimatic Interpretation of a Continuous 7.2 Ma Late Cenozoic Eolian Sediments from the Chinese Loess Plateau. Geophysical Research Letters, 25(1): 85-88. doi: 10.1029/97gl03353
      Sun, J.Z., 2005. Loessology. Hong Kong Archaeological Society Press, Hong Kong, 354-362(in Chinese).
      Sun, J., Z., Wang, Y., Z., Zhang, Q., Y., 1982. Various Geochronology of Quaternary Stratigraphy in Songliao Plain. Journal of Xi'an Institute of Geology, (2): 79-91, 10(in Chinese).
      Wan, B., Zhong, Y.Z., 1997. Features Analysis and Divisions of New Tectonic Movement in Northeast China. Seismological Research of Northeast China, (4): 64-75(in Chinese). http://www.researchgate.net/publication/285021690_Features_analysis_and_divisions_of_new_tectonic_movement_in_northeast_China
      Wang, D.P., Wang, X.K., Jiang, Y.B., 2010. Reconstruction of the Paleo-Environment in Changchun Area, Northeast China during the Late Mid-Pleistocene: Evidences from Sedimentary Geochemistry and Palynology. Journal of Jilin University: Earth Science Edition, 40(5): 1066-1074(in Chinese with English abstract). doi: 10.3969/j.issn.1671-5888.2010.05.013
      Wang, J.L., 1993. Study on the Harbin Section of Songhua River terrace. Scientia Geographica Sinica, 13(1): 87-90(in Chinese).
      Wei, Q., 1979. The Straigraphy and the Age of the Huangshan in Harbin. Acta Stratigraphica Sinica, 3: 208-213(in Chinese).
      Wu, X.H., Pu, Q.Y., Qian, F., et al., 1984. Preliminary Study on the Quaternary Magnetostratigraphy of the Songliao Plain in North-East China. Marine Geology & Quaternary Geology, 4(2): 1-13 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-HYDZ198402000.htm
      Xia, Y.M., Wang, P.F., Wang, M.H., 1983. Priliminary Research on Spore-Pollen Association of the Section of Huang Shan in Haerbin. Scientia Geographica Sinica, 3(2): 183-187, 192 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DLKX198302012.htm
      Xie, Y.Y., He, K., Kang, C.G., 2005. Grain-Size Distribution of Fall-Outs of an Exceedingly Large Dust Storm in Harbin City and Its Implications. Geology in China, 32(3): 502-506(in Chinese with English abstract). doi: 10.3969/j.issn.1000-3657.2005.03.021
      Yi, S.W., Lu, H.Y., Zhou, Y.L., et al., 2013. Rb/Sr Geochemistry of Loess Deposits in the Horqin Dunefield, Northeastern China, and Its Implications for Climate Change during Late Quaternary. Marine Geology & Quaternary Geology, 33(2): 129-136 (in Chinese with English abstract). http://adsabs.harvard.edu/abs/2014MGQG...33..129Y
      Zeng, L., Lu, H.Y., Yi, S.W., et al., 2011. Magnetostratigraphy of Loess in Northeastern China and Paleoclimatic Changes. Chinese Science Bulletin, 56(27): 2267-2275 (in Chinese with English abstract). doi: 10.1360/972011-311
      Zhang, W., Guo, S.L., Li, Y.H., et al., 2010. Grain-Size Fractal Dimension of Loess and Its Environmental Significance in the Peninsula of East Liaoning. Progress in Geography, 29(1): 79-86(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DLKJ201001014.htm
      Zhang, W., Li, Y.Y., Li, L., 2008. Study on Loess Granularity and Sedimentary Environment at Qidingshan in Dalian. Resources & Industries, 10(3): 75-80(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZIYU200803021.htm
      Zheng, X.M., Liu, F., 2006. Review of Reseach on Loess in the Yangtze River Delta and the East China Sea Islands. Journal of East China Normal University: Natural Science, (6): 9-24(in Chinese with English abstract). doi: 10.3969/j.issn.1000-5641.2006.06.002
      Zhu, R., X., Kazansky, A., Matasova, G., et al., 2000. The magnetic properties of the loess deposits in southern Siberia. Chinese Science Bulletin, 11: 1200-1205(in Chinese).
      帕夫林诺夫, B.H., 于丕休, 石世民, 等, 1956. 关于中国黄土的成因问题. 科学通报, 1(11): 1-15. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB195611000.htm
      蔡茂堂, 魏明建, 2009. 洛川地区倒数第二次间冰期气候变化研究. 中国沙漠, 29(3): 536-543. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGSS200903027.htm
      曹振, 朱晓东, 2014. 东北地区中、东部黄土成因初步研究. 长春师范学院学报: 自然科学版, (2): 85-89. https://www.cnki.com.cn/Article/CJFDTOTAL-CCSS201404024.htm
      曾琳, 鹿化煜, 弋双文, 等, 2011. 我国东北地区黄土堆积的磁性地层年代与古气候变化. 科学通报, 56(27): 2267-2275. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201127002.htm
      初本君, 高振操, 杨世生, 等, 1988. 松嫩平原第四纪磁性地层的初步划分. 海洋地质与第四纪地质, 8(4): 91-96. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198804014.htm
      何葵, 康春国, 张丽娟, 2008. 松花江哈尔滨段河床冲积物与沙尘天气关系的讨论. 中国地质, 35(1): 150-156. doi: 10.3969/j.issn.1000-3657.2008.01.016
      何葵, 谢远云, 康春国, 等, 2009. 哈尔滨沙尘沉降物的粒度组成及其源地分析. 中国农学通报, 25(11): 200-205. https://www.cnki.com.cn/Article/CJFDTOTAL-ZNTB200911044.htm
      何葵, 谢远云, 张丽娟, 等, 2005. 哈尔滨2002年3月20日沙尘暴沉降物的粒度特征及其意义. 地理科学, 25(5): 597-600. doi: 10.3969/j.issn.1000-0690.2005.05.014
      胡碧茹, 卢演俦, 1989. 洛川黄土剖面的粉砂与粘粒比值及粒度旋回. 岩石学报, 5(1): 12-20. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB198901001.htm
      康春国, 李长安, 谢远云, 等, 2011. 哈尔滨地区风尘黄土重矿物特征及物源分析. 自然灾害学报, 20(4): 43-51. https://www.cnki.com.cn/Article/CJFDTOTAL-ZRZH201104006.htm
      李崇银, 王作台, 林士哲, 等, 2004. 东亚夏季风活动与东亚高空西风急流位置北跳关系的研究. 大气科学, 28(5): 641-658. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200405000.htm
      李丽, 2009. 大连地区滨海黄土古环境信息研究(硕士学位论文). 辽宁: 辽宁师范大学, 1-51.
      李徐生, 杨达源, 鹿化煜, 2001. 镇江下蜀黄土粒度特征及其成因初探. 海洋地质与第四纪地质, 21(1): 25-32. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200101005.htm
      李雪铭, 2001. 辽东半岛南部地区滨海黄土的沉积特征. 海洋科学, 25(1): 32-35. https://www.cnki.com.cn/Article/CJFDTOTAL-HYKX200101011.htm
      李长安, 张玉芬, 袁胜元, 等, 2010. "巫山黄土"粒度特征及其对成因的指示. 地球科学——中国地质大学学报, 35(5): 879-884. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201005018.htm
      刘东生, 安芷生, 郑洪汉, 1985. 黃土与环境. 北京: 科学出版社, 191-379.
      刘东生, 丁仲礼, 郭正堂, 等, 1991. 黄土与干旱环境. 安徽: 安徽科学出版社, 34-278.
      刘庆宏, 贾亮, 2010. 大连滨海七顶山黄土沉积学特点分析. 辽宁师专学报: 自然科学版, (2): 50-51, 89. https://www.cnki.com.cn/Article/CJFDTOTAL-LAON201002034.htm
      刘秀铭, 刘东生, 夏敦胜, 等, 2007b. 中国与西伯利亚黄土磁化率古气候记录——氧化和还原条件下的两种成土模式分析. 中国科学(D辑), 37(10): 1382-1391. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200710012.htm
      刘秀铭, 夏敦胜, 刘东生, 等, 2007a. 中国黄土和阿拉斯加黄土磁化率气候记录的两种模式探讨. 第四纪研究, 27(2): 210-220. https://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200702005.htm
      鹿化煜, 安芷生, 1999. 黄土高原红粘土与黄土古土壤粒度特征对比——红粘土风成成因的新证据. 沉积学报, 17(2): 61-67. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB902.010.htm
      吕金福, 李志民, 1990. 辽东半岛的黄土及其沉积环境. 地理科学, 10(2): 97-106, 191. https://www.cnki.com.cn/Article/CJFDTOTAL-DLKX199002000.htm
      任剑璋, 全浩, 丁仲礼, 等. 1997. 倒数第二次冰期气候快速变化的一个例证: 会宁黄土的气候不稳定性记录. 科学通报, 42(17): 1836-1839. doi: 10.3321/j.issn:0023-074X.1997.17.013
      任少芳, 郑祥民, 艾东升, 等, 2014. 不同前处理方法对下蜀黄土粒度测量的影响. 海洋地质与第四纪地质, (3): 185-194. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201403027.htm
      孙东怀, 鹿化煜, 2007. 晚新生代黄土高原风尘序列的粒度和沉积速率与中国北方大气环流演变. 第四纪研究, 27(2): 251-262. doi: 10.3321/j.issn:1001-7410.2007.02.010
      孙东怀, 鹿化煜, David R., 等, 2000. 中国黄土粒度的双峰分布及其古气候意义. 沉积学报, 18(3): 327-335. doi: 10.3969/j.issn.1000-0550.2000.03.001
      孙建中, 2005. 黄土学. 香港: 香港考古学会出版社, 354-362.
      孙建中, 王雨灼, 张庆云, 1982. 松辽平原第四纪地层的划分——几种年代学方法的应用. 长安大学学报: 地球科学版, (2): 79-91, 10. https://www.cnki.com.cn/Article/CJFDTOTAL-XAGX198202011.htm
      万波, 钟以章, 1997. 东北地区的新构造运动特征分析及新构造运动分区. 东北地震研究, (4): 64-75. https://www.cnki.com.cn/Article/CJFDTOTAL-DDYJ704.008.htm
      王丹萍, 王锡魁, 江裕标, 2010. 长春地区中更新世晚期古环境重建的沉积地球化学与孢粉学证据. 吉林大学学报: 地球科学版, 40(5): 1066-1074. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201005015.htm
      王璟璐, 1993. 松花江哈尔滨段阶地的研究. 地理科学, 13(1): 87-90. https://www.cnki.com.cn/Article/CJFDTOTAL-DLKX199301012.htm
      卫奇, 1979. 哈尔滨黄山地层的时代. 地层学杂志, 3(3): 208-213. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ197903006.htm
      吴锡浩, 浦庆余, 钱方, 等, 1984. 松辽平原第四纪磁性地层的初步研究. 海洋地质与第四纪地质, 4(2): 1-13. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198402000.htm
      夏玉梅, 汪佩芳, 王曼华, 1983. 哈尔滨黄山剖面孢粉组合的初步研究. 地理科学, 3(2): 183-187, 192. https://www.cnki.com.cn/Article/CJFDTOTAL-DLKX198302012.htm
      谢远云, 何葵, 康春国, 2005. 哈尔滨市特大沙尘暴沉降物的粒度分布及意义. 中国地质, 32(3): 502-506. doi: 10.3969/j.issn.1000-3657.2005.03.021
      弋双文, 鹿化煜, 周亚利, 等, 2013. 晚第四纪科尔沁黄土堆积的Rb-Sr地球化学特征及古气候变化. 海洋地质与第四纪地质, 33(2): 129-136. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201302021.htm
      张威, 郭善莉, 李永化, 等, 2010. 辽东半岛黄土粒度分维特征及其环境意义. 地理科学进展, 29(1): 79-86. https://www.cnki.com.cn/Article/CJFDTOTAL-DLKJ201001014.htm
      张威, 李云艳, 李丽, 2008. 大连市七顶山黄土粒度特征及其沉积环境. 资源与产业, 10(3): 75-80. doi: 10.3969/j.issn.1673-2464.2008.03.019
      郑祥民, 刘飞, 2006. 长江三角洲与东海岛屿黄土研究综述. 华东师范大学学报: 自然科学版, (6): 9-24. https://www.cnki.com.cn/Article/CJFDTOTAL-HDSZ200606001.htm
      朱日祥, Kazansky, A., Matasova, G., 等, 2000. 西伯利亚南部黄土沉积物的磁学性质. 科学通报, 45(11): 1200-1205. doi: 10.3321/j.issn:0023-074X.2000.11.017
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