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    洞庭盆地S3-7孔第四纪年代地层

    赵举兴 李长安 张玉芬 强小科 熊德强

    赵举兴, 李长安, 张玉芬, 强小科, 熊德强, 2016. 洞庭盆地S3-7孔第四纪年代地层. 地球科学, 41(4): 633-643. doi: 10.3799/dqkx.2016.052
    引用本文: 赵举兴, 李长安, 张玉芬, 强小科, 熊德强, 2016. 洞庭盆地S3-7孔第四纪年代地层. 地球科学, 41(4): 633-643. doi: 10.3799/dqkx.2016.052
    Zhao Juxing, Li Chang'an, Zhang Yufen, Qiang Xiaoke, Xiong Deqiang, 2016. Quaternary Chronostratigraphy of Borehole S3-7 in Dongting Basin. Earth Science, 41(4): 633-643. doi: 10.3799/dqkx.2016.052
    Citation: Zhao Juxing, Li Chang'an, Zhang Yufen, Qiang Xiaoke, Xiong Deqiang, 2016. Quaternary Chronostratigraphy of Borehole S3-7 in Dongting Basin. Earth Science, 41(4): 633-643. doi: 10.3799/dqkx.2016.052

    洞庭盆地S3-7孔第四纪年代地层

    doi: 10.3799/dqkx.2016.052
    基金项目: 

    国家自然科学基金项目 41440002

    中国地质调查局项目 1212011121142

    详细信息
      作者简介:

      赵举兴(1986-),男,博士生,主要从事第四纪地质学方面的研究. E-mail: zhaojuxing1986@126.com

      通讯作者:

      张玉芬, E-mail: zhyfcug@163.com

    • 中图分类号: P642.22

    Quaternary Chronostratigraphy of Borehole S3-7 in Dongting Basin

    • 摘要: 洞庭盆地的形成与演化对长江中游乃至中国中部的地质环境变迁具有重要意义,但区内的第四纪年代地层研究一直不足.以洞庭盆地沉积中心——沅江凹陷的典型钻孔S3-7孔(孔深255.1 m)为研究对象,在详细的沉积物岩性描述和岩石地层划分的基础上,系统地进行了古地磁、ESR、AMS14C等测试,并建立了S3-7孔的年代地层序列.通过与其他两口典型钻孔的对比分析,初步建立了研究区的区域年代地层格架,结果显示洞庭盆地沉积中心下更新统底界位于各钻孔底部240~300 m,中更新统底界位于90~95 m,上更新统底界位于28~50 m,全新统底界位于1.5~3.1 m.平均沉积速率和分段线性方程的结果表明洞庭盆地覆盖第四纪区岩石地层单位的时代为:华田组的地质年龄为2 590~1 600 ka BP,湘阴组的地质年龄为1 600~920 ka BP,洞庭湖组的地质年龄为920~120 ka BP,安乡组的地质年龄为120~11 ka BP,全新统的地质年龄为11 ka BP至今.

       

    • 图  1  洞庭盆地典型钻孔位置

      Fig.  1.  Location of typical boreholes in the Dongting basin

      图  2  洞庭盆地第四系划分

      括号内为各岩石地层单位代号.《湖南省区域地质志》对洞庭盆地第四系只划分了更新统和全新统,并未将更新统三分,同时该专著中未系统列出各岩石地层代号

      Fig.  2.  Division of Quaternary in the Dongting basin

      图  3  S3-7孔综合地层划分

      Fig.  3.  Division of integrated stratigraphy in the borehole S3-7

      图  4  安乡凹陷-沅江凹陷地层对比

      为统一对比,本文将ZKC01孔(柏道远,2010)的坡头组改为安乡组;将ZK1孔(张建新等,2007)全新世团州组和赤沙组合并为全新统;由于S3-7孔与ZK1孔下伏基岩为小木坪组,ZKC01孔下伏基岩为马底驿组,图中未标出华田组下段的下伏岩石地层单位

      Fig.  4.  Stratigraphic correlation of Anxiang and Yuanjiang depression

      表  1  洞庭盆地覆盖区第四纪岩石地层单位划分及主要岩性特征

      Table  1.   Division and characteristics of Quaternary lithostratigraphical units in the Dongting basin coverage area

      地层 组(代号) 主要岩性特征
      全新统 未分组(Qh) 青灰、褐黄色、灰黑色黏土、粉砂及细砂层,偶见砾石,个别地层含螺蚌壳化石及含腐殖物残骸炭化木;一般厚度小于25 m.
      上更新统 安乡组(Qp3a) 总体颜色为褐黄色,上部为褐黄色黏土、粉砂及细砂层,下部为含细砾砂层,未经暴露的可能为青灰色,含铁锰薄膜或结核;厚度可达20~30 m.
      中更新统 洞庭湖组上段(Qp2dt3) 总体颜色为褐黄色,上部为褐黄、灰黑色黏土、粉砂,下部为褐黄色、灰色含砾砂层、砾石层;一般厚20 m,个别可达50 m.
      洞庭湖组中段(Qp2dt2) 总体颜色为黄-褐黄色,上部为褐黄、灰黑色黏土、粉砂,下部为褐黄色、灰色含砾砂层、砾石层,通常由两期沉积旋回构成;一般厚20 m,个别可达80 m.
      洞庭湖组下段(Qp2dt1) 总体颜色为褐黄-青灰色,上部为灰绿、绛红色黏土、粉砂,下部为褐黄色、灰色含砾砂层、砾石层一般厚30 m,个别可达90 m.
      下更新统 湘阴组(Qp1xy) 总体颜色为青灰色,上部为灰绿、灰黑色黏土、粉砂,下部为褐灰色、灰色含砾砂层、砾石层;一般厚60 m,个别可达100 m.
      华田组上段(Qp1ht2) 总体颜色为青灰色,上部为以绛红色为主的杂色黏土,下部为褐灰色、灰色含砾砂层、砾石层;杂色黏土是与湘阴组的分层标志;一般厚40~60 m,个别可达100 m.
      华田组下段(Qp1ht1) 总体颜色为青灰色,上部为以绛红色、灰绿色为主的杂色黏土,下部为褐灰色、灰色含砾砂层、砾石层;出现大量炭化木碎屑;一般厚30~40 m,个别可达100 m.
      下载: 导出CSV

      表  2  S3-7孔第四纪岩石地层及沉积环境

      Table  2.   Quaternary lithostratigraphical units and sedimentary environments of the borehole S3-7

      地质时代 岩石地层 代号 地层特征及沉积序列
      全新世 全新统 Qh 包括最顶部的1个岩性层,由一期沉积旋回组成,与下伏安乡组假整合接触.底部为褐黄色粉砂质黏土与青灰色黏土互层,顶部为浅褐色粉砂质黏土层.沉积环境由缓流的河漫滩沉积到静水湖沼沉积.厚3.04 m
      更新世 安乡组 Qp3a 包括2~6等5个岩性层,由一期沉积旋回组成,与下伏洞庭湖组假整合接触.底部为浅青灰色细砾石层,略显正粒序结构;中部为褐黄色细-中砂层;顶部为褐黄色黏土质粉砂层,见铁锰结核.沉积环境由河流沉积逐渐过渡为缓流或静水湖相沉积.厚25.46 m
      洞庭湖组上段 Qp2dt3 包括7~12等6个岩性层,由三期沉积旋回组成.底部为黄-褐黄色含细砾粗砂层,上覆褐黄色粗砂层;中部为黄色含细砾粗砂层,上覆褐黄色、绛红色黏土互层;顶部为深褐黄色细砾石层,上覆浅褐黄色含砾粗砂层.该段出现较厚的砾石层,反映出河流水动力的增强.厚31.41 m
      洞庭湖组中段 Qp2dt2 包括13~16等4个岩性层,由两期沉积旋回组成.底部为褐黄色含细砾粗砂层,上覆粉红、浅紫色为主的杂色黏土与粉砂质黏土互层,偶见铁壳;中部为褐黄色含砾中-粗砂层;顶部为褐黄色中-粗砂层.中段含砾砂层厚度明显增大,反映该段水动力一直较强.厚23.82 m
      洞庭湖组下段 Qp2dt1 包括17~23等7个岩性层,由三期沉积旋回组成.底部为褐黄-青灰色含细砾粗砂层,偶见白云母碎片,上覆褐黄-青灰色细砂层及黏土层;中部为褐黄-青灰色含细砾中-粗砂层,夹褐黄色、灰黑色、黑绿色花纹;顶部为绛红色、褐黄色、青灰色黏土互层.三期沉积旋回中沉积物的二元结构明显,为典型的河流沉积,同时三期沉积旋回底部均为含砾粗砂,向上为中-粗砂或黏土,反映经历了三期下部为河流急流相沉积而顶部缓流或静水沉积.厚24.81 m
      湘阴组 Qp1xy 包括24~30等7个岩性层,由四期沉积旋回组成,与下伏华田组整合接触.底部为青灰色细-中砂层,见大量白云母碎片,上覆青灰色粉砂质黏土层;中部为青灰色、褐黄色含细砾粗砂层,偶见白云母碎片;顶部为青灰色中-粗砂层,多见白云母碎片与铁锰结核.总体上为河流沉积为主的河湖交替的沉积环境.厚66.00 m
      华田组上段 Qp1ht2 包括31~35等5个岩性层,由两期沉积旋回组成.底部为青灰色含细砾中-粗砂,上覆青灰色、黑灰色粉砂与杂色粉砂质黏土互层;中部为青灰色、褐黄色含细砾细砂层,偶见白云母碎片;顶部为绛红色为主的杂色粉砂质黏土与黏土互层,偶见铁壳.该段同样为河湖频繁交替的沉积特征.厚34.74 m
      华田组下段 Qp1ht1 包括36~39等4个岩性层,由两期沉积旋回组成.底部为青灰色细砂层,上覆绛红色为主的杂色粉砂质黏土与黏土互层,见大量铁锰结核;中部为青灰色细砂层,多见炭化木块;顶部为青灰色、灰黑色粉砂质黏土互层,偶见炭化木块.该段的沉积环境大致经历了河流相→湖泊相→河流相→湖泊相的演变.厚35.35 m
      下载: 导出CSV

      表  3  S3-7孔AMS 14C测试结果

      Table  3.   Dating results of AMS 14C in the borehole S3-7

      样品编号 深度(m) 测试材料 14C年龄(a BP) 校正年龄±1δ(a BP) 校正年龄±2δ(a BP)
      14C-1 1.5 黏土 2 720±30 2 814±32 2 818±58
      14C-2 1.8 黏土 3 350±30 3 860±33 3 868±57
      14C-3 3.8 黏土 14 850±70 18 386±84 17 973±203
      14C-4 13.3 黏土 20 810±890 24 918±1 139 24 810±7 040
      下载: 导出CSV

      表  4  S3-7孔ESR测年结果

      Table  4.   Dating results of ESR in the borehole S3-7

      样品编号 深度(m) 测试材料 ED(Gy) D(Gy/ka) 年龄(ka BP)
      ESR-1 54.4 细砂 624.6±61.0 4.364 143±14
      ESR-2 68.4 细砂 927.6±78.0 3.910 237±20
      ESR-3 83.3 细砂 920.5±92.0 2.187 421±42
      ESR-4 103.0 细砂 4 060.6±397.0 4.960 819±80
      ESR-5 123.6 细砂 4 177.8±391.0 3.914 1 068±100
      ESR-6 144.5 细砂 5 587.5±540.0 4.912 1 137±110
      ESR-7 200.6 细砂 5 890.6±468.0 3.120 1 888±150
      ESR-8 223.8 细砂 8 425.5±746.0 3.732 2 258±200
      ESR-9 240.7 细砂 8 900.0±762.0 3.809 2 337±200
      下载: 导出CSV

      表  5  各年代地层底界在典型钻孔中的位置

      Table  5.   Boundaries of chronostratigraphy in typical boreholes

      钻孔 位置 全新统孔深(m) 上更新统孔深(m) 中更新统孔深(m) 下更新统孔深(m)
      ZKC01 安乡凹陷 1.50 28.00 92.00 294.24
      ZK1 沅江凹陷 1.60 12.00 95.00 270.68
      S3-7 沅江凹陷 3.10 50.00 90.00 244.63
      下载: 导出CSV
    • Bai, D.Y., 2010.Quaternary Geological and Environmental Evolution of the Dongting Basin (Dissertation).China University of Geosciences, Wuhan, 41-49(in Chinese with English abstract). doi: 10.1007%2F978-3-642-17220-5_2
      Bai, D.Y., Li, C.A., Zhou, K.J., et al., 2010a.Geological Characteristics and Tectonic-Sedimentary Coupling Relation of the Chishan Uplift and Anxiang Sag of Quaternary Dongting Basin.Acta Sedimentologica Sinica, 28(4):645-658 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB201004000.htm
      Bai, D.Y., Li, S.W., Zhou, K.J., et al., 2010b.Tectonic-Sedimentary Landform Classification of 1:250 000 Changde Sheet and Its Implication for Researches on Quaternary Geology and Environment of Jianghan-Dongting Basin.Geology in China, 37(2):280-297(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-DZWZ201101026.htm
      Bai, D.Y., Wang, X.H., Li, C.A., et al., 2011.Characteristics of Quaternary Tectonic Evolution in Dongting Basin.Geological Review, 57(2):261-276(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP201102014.htm
      Bureau of Geology and Mineral of Hunan Province, 1988.Regional Geology of Hunan Province.Geological Publishing House, Beijing, 263(in Chinese with English abstract). https://www.deepdyve.com/lp/elsevier/paleomagnetism-of-middle-triassic-redbeds-from-hubei-and-northwestern-0UU0Sec0Vr
      Cai, S.M., Guan, Z.H., Kong, Z.C., et al., 1984.Natural Environment as Reflected in Sedimentary Facies and Sporo-Pollen Assemblages in Dongting Basin in Quaternary.Oceanologia et Limnologia Sinica, 15(6):527-539(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DLXB198704001.htm
      Chen, C.M., Xie, B.G., 1996.Stratigraphical Division and Lower Limit of the Quaternary in Hunan.Journal of Stratigraphy, 20(4):271-276(in Chinese with English abstract). http://linkinghub.elsevier.com/retrieve/pii/S0016787863800310
      Chen, D.P., Li, C.A., Bai, D.Y., et al., 2014.Preliminary Discussion on the Quaternary Stratigraphic Framework of Dongting Basin.Geological Science and Technology Information, 33(1):67-73(in Chinese with English abstract). https://pubs.er.usgs.gov/publication/ofr84413
      Du, Y., Yin, H.F., 2003.Study on Historical Environment in Dongting Lake Area.Earth Science, 28(2):214-218(in Chinese with English abstract). https://www.researchgate.net/publication/297705120_Study_on_historical_environment_in_Dongting_Lake_area
      Editorial Board of Stratigraphical Lexicon of China, 2000.Stratigraphical Lexicon of China, Quaternary.Geological Publishing House, Beijing, 62 (in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DSJJ199903010.htm
      Jing, C.Y., 1982.The Formation and Evolution of Dongting Lake.Journal of Nanjing Normal University (Natural Science Edition), 2:52-60(in Chinese). http://www.oalib.com/paper/1562784
      Lai, H.Z., Mo, D.W., 2004.Influences of the Tectonic Subsidence and the Siltation on Flood Disaster Prevention Situation in the Region of Dongting Lake.Acta Geographica Sinica, 59(4):574-580(in Chinese with English abstract). https://www.researchgate.net/publication/226036870_Influences_of_the_tectonic_subsidence_and_the_siltation_on_flood_disaster_prevention_situation_in_the_region_of_Dongting_Lake
      Lai, H.Z., Mo, D.W., Li, X.B., 2005.Research on the Quaternary Laterite and Paleoclimate in the Dongting Basin.Acta Sedimentologica Sinica, 23(1):130-137(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB20050100G.htm
      Li, C.A., 1998.Some Problems on Study of the Quaternary Stratigrahy in China.Journal of Stratigraphy, 23(4):287-290(in Chinese with English abstract). http://www.sciencedirect.com/science/article/pii/0277379186902167/part/first-page-pdf
      Li, C.A., 2002.Report of the Flood Area in the Middle Reach of Yangtze River—Division of the Quaternary Strata.China University of Geosciences, Wuhan (in Chinese). doi: 10.1007/978-4-431-55245-1_4/fulltext.html
      Li, C.A., 2015.The Relationship among Human, Water and Land:Optimizing Function of the Embankment in the Yangtze River.Earth Science, 40(2):261-267 (in Chinese with English abstract). doi: 10.1007/s00267-015-0642-6
      Li, C.A., Zhang, Y.F., Pi, J.G., et al., 2006.Discovery and Significance of Paleo-Lakeside Gravel Layer on Dongting Basin.Quaternary Sciences, 26(3):491-492(in Chinese). http://www.academia.edu/9203597/Paleolandscape_variation_and_Early_Pleistocene_hominid_activities_Members_1_and_7_Olorgesailie_Formation_Kenya
      Lisiecki, L.E., Raymo, M.E., 2005.A Pliocenee-Pleistocene Stack of 57 Globally Distributed Benthic δ18O Records.Paleoceanography, 20(1):PA1003. http://www.nature.com/ngeo/journal/v10/n4/full/ngeo2914.html
      Liu, C.R., Yin, G.M., Gao, L., et al., 2011.Research Advances in ESR Geochronology of Quaternary Deposits.Seismology and Geology, 33(2):490-498(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZDZ201102027.htm
      Mao, L.J., Mo, D.W., Yang, J.H., et al., 2008.Rare Earth Element Geochemistry of Reticulate Red Clay around Dongting Lake.Environmental Chemistry, 27(2):222-225(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HJHX200802023.htm
      Pi, J.G., Liu, C.M., He, J.J., et al., 2002.Environmental and Geological Report of the Dongting Lake in the Middle Reach of Yangtze River.Hunan Institute of Geological Survey, Changsha, 19-33 (in Chinese). https://www.deepdyve.com/lp/elsevier/interpretation-of-the-environmental-change-of-dongting-lake-middle-z5YKNL89Mg
      Pi, J.G., Zhang, G.L., 1993.Research of Analysis Method of Sedimentary Environment in Dongting Lake Basin.Hunan Geology, 12(3):196-199 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HNDZ199303012.htm
      Pi, J.G., Zhang, G.L., Liang, X., et al., 2001.Preliminary Research on Sedimentary Environment Evolution in Dongting Basin in the Quaternary Period.Geological Science and Technology Information, 20(2):6-10 (in Chinese with English abstract). https://www.researchgate.net/publication/293344071_Preliminary_research_on_sedimentary_environment_evolution_in_Dongting_Basin_in_the_Quaternary_Period
      Qiang, X.K., An, Z.S., Song, Y.G., et al., 2010.New Eolian Red Clay Sequence on the Western Chinese Loess Plateau Linked to Onset of Asian Desertification about 25 Ma Ago.Science in China (Series D), 54(1):136-144 (in Chinese). doi: 10.1007/s11430-010-4126-5
      Reimer, P.J., Baillie, M.G.L., Bard, E., et al., 2009.IntCal09 and Marine09 Radiocarbon Age Calibration Curves, 0-50 000 Years cal BP.Geochemistry & Geophysics, 51(4):1111-1150. https://journals.uair.arizona.edu/index.php/radiocarbon/article/viewFile/3569/3082
      Su, C., Mo, D.W., Wang, H., 2001.Evolution of Lake Dongting and Its Flood Disasters.Research of Soil and Water Conservation, 8(2):52-55(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-STBY200102014.htm
      Wang, C.L., 1992.Formation and Evolution of the Dongting Basin.Geotectonica et Metallogenia, 16(1):98-99 (in Chinese). https://www.researchgate.net/publication/284686091_Formation_and_evolution_of_the_Datong-Yangyuan_basin
      Xiong, D.Q., 2014.Quaternary Magnetic Stratigraphy and Paleoenvironment in Dongting Basin(Dissertation).China University of Geosciences, Wuhan, 26-36(in Chinese with English abstract). http://www.sciencedirect.com/science/article/pii/B9780444536433000650
      Xu, J.X., 2007.A Study of Depositional Rate in the North China Plain during the Past 40 000 Years Based on 14C Dating Data from a Large Wealth of Samples.Quaternary Sciences, 27(3):437-443 (in Chinese with English abstract). https://www.researchgate.net/publication/289074356_The_Stratigraphic_Evolution_of_the_Sunda_Shelf_during_the_Past_Fifty_Thousand_Years
      Yang, D.Y., 1986.On the Evolution of the Dongting Lake during Holocene and the Way of Management.Geographical Research, 5(3):39-46 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DLYJ198603003.htm
      Zhang, G.L., Pi, J.G., Sun, X.L., et al., 1990.Quaternary Report of the Dongting Basin in Hunan Province.Hunan Institute of Geological Prospect, Changsha, 16-49 (in Chinese). https://www.researchgate.net/publication/294549479_The_tectogenesis_in_the_Quaternary_period_of_the_Dongting_Basin
      Zhang, J.X., Shen, Z.J., Gu, H.B., et al., 2007.Quaternary Environmental Geochemistry of Dongting Basin.Geological Publishing House, Beijing, 28-44 (in Chinese). http://or.nsfc.gov.cn/handle/00001903-5/51582
      Zhang, R.Q., Liang, X., Zhang, G.L., et al., 2001.A Preliminary Study of Climate Change in Dongting Lake Area in the Quaternary Period.Geological Science and Technology Information, 20(2):1-5 (in Chinese with English abstract). http://linkinghub.elsevier.com/retrieve/pii/S2210784310000057
      Zhang, X.Y., Cai, S.M., Sun, S.C., 1994.Evolution of Dongting Lake since Holocene.Journal of Lake Sciences, 6(1):13-21 (in Chinese with English abstract). doi: 10.18307/1994.0102
      Zhao, J.X., Li, C.A., Xu, Y.S., 2014.Sedimentary Characteristics and Sedimentary Environment of the Gravel Bed within Paleo-Yuanjiang River from Dongting Basin.Geological Science and Technology Information, 33(1):85-89 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DLKX201606019.htm
      柏道远, 2010.洞庭盆地第四纪地质环境演化(博士学位论文).武汉:中国地质大学, 41-49. http://cdmd.cnki.com.cn/Article/CDMD-10674-2004102550.htm
      柏道远, 李长安, 周柯军, 等, 2010a.第四纪洞庭盆地赤山隆起与安乡凹陷升降运动的沉积记录.沉积学报, 28(4): 645-658. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201004000.htm
      柏道远, 李送文, 周柯军, 等, 2010b.1:25万常德市幅构造-沉积地貌类型划分及其对江汉-洞庭盆地第四纪地质与环境研究的启示.中国地质, 37(2): 280-297. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201002004.htm
      柏道远, 王先辉, 李长安, 等, 2011.洞庭盆地第四纪构造演化特征.地质评论, 57(2): 261-276. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201102014.htm
      湖南省地质矿产局, 1988.湖南省区域地质志.北京:地质出版社, 263. http://www.cnki.com.cn/Article/CJFDTOTAL-TTSD199206004.htm
      蔡述明, 官子和, 孔昭宸, 等, 1984.从岩相特征和孢粉组合探讨洞庭盆地第四纪自然环境的变迁.海洋与湖沼, 15(6): 527-539. http://www.cnki.com.cn/Article/CJFDTOTAL-HYFZ198406003.htm
      陈长明, 谢丙庚, 1996.湖南第四纪地层划分及其下限.地层学杂志, 20(4): 271-276. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ604.004.htm
      陈渡平, 李长安, 柏道远, 等, 2014.洞庭盆地第四纪地层格架初拟.地质科技情报, 33(1): 67-73. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201401011.htm
      杜耘, 殷鸿福, 2003.洞庭湖历史时期环境研究.地球科学, 28(2): 214-218. http://earth-science.net/WebPage/Article.aspx?id=1239
      《中国地层典》编委会, 2000.中国地层典——第四系.北京:地质出版社, 62. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ199201007.htm
      景存义, 1982.洞庭湖的形成与演变.南京师院学报(自然科学版), 2: 52-60. http://www.cnki.com.cn/Article/CJFDTOTAL-NSYJ198601007.htm
      来红州, 莫多闻, 2004.构造沉降和泥沙淤积对洞庭湖区防洪的影响.地理学报, 59(4): 574-580. doi: 10.11821/xb200404011
      来红州, 莫多闻, 李新坡, 2005.洞庭盆地第四纪红土层及古气候研究.沉积学报, 23(1): 130-137. http://www.cnki.com.cn/Article/CJFDTOTAL-TTSD200904003.htm
      李长安, 1999.中国第四纪地层研究中的若干问题.地层学杂志, 23(4): 287-290. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ199904007.htm
      李长安, 2002.长江中游水患区报告——第四纪地层的划分.武汉:中国地质大学. http://www.doc88.com/p-353268286302.html
      李长安, 2015.基于"人-水-地和谐"的长江堤防功能.地球科学, 40(2): 261-267. http://earth-science.net/WebPage/Article.aspx?id=3049
      李长安, 张玉芬, 皮建高, 等, 2006.洞庭湖古湖滨砾石层的发现及意义.第四纪研究, 26(3): 491-492. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200603023.htm
      刘春茹, 尹功明, 高璐, 等, 2011.第四纪沉积物ESR年代学研究进展.地震地质, 33(2): 490-498. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201102027.htm
      毛龙江, 莫多闻, 杨兢红, 等, 2008.环洞庭湖地区网纹红土中稀土元素的地球化学特征.环境化学, 27(2): 222-225. http://www.cnki.com.cn/Article/CJFDTOTAL-HJHX200802023.htm
      皮建高, 刘长明, 何建军, 等, 2002.长江中游洞庭湖水患区环境地质调查评价报告.长沙:湖南省地质调查院, 19-33. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ200400005012.htm
      皮建高, 张国梁, 1993.洞庭湖盆地沉积环境分析方法探索.湖南地质, 12(3): 196-199. http://www.cnki.com.cn/Article/CJFDTOTAL-HNDZ199303012.htm
      皮建高, 张国梁, 梁杏, 等, 2001.洞庭盆地第四纪沉积环境演变的初步分析.地质科技情报, 20(2): 6-10. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200102001.htm
      强小科, 安芷生, 宋友桂, 等, 2010.晚渐新世以来中国黄土高原风成红粘土序列的发现:亚洲内陆干旱化起源的新记录.中国科学(D辑), 40(11): 1479-1488. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201011003.htm
      苏成, 莫多闻, 王辉, 2001.洞庭湖的形成、演变与洪涝灾害.水土保持研究, 8(2): 52-55. http://www.cnki.com.cn/Article/CJFDTOTAL-STBY200102014.htm
      王春林, 1992.洞庭盆地的形成和演化.大地构造与成矿学, 16(1): 98-99. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK199201023.htm
      熊德强, 2014.洞庭盆地第四纪磁性地层与古环境(硕士学位论文).武汉:中国地质大学, 26-36. http://cdmd.cnki.com.cn/Article/CDMD-10112-2003094150.htm
      许炯心, 2007.基于大样本14C测年资料的华北平原沉积速率研究.第四纪研究, 27(3): 437-443. http://www.cqvip.com/QK/97036X/200703/24511975.html
      杨达源, 1986.洞庭湖的演变及其整治.地理研究, 5(3): 39-46. http://www.cnki.com.cn/Article/CJFDTOTAL-DLYJ198603003.htm
      张国梁, 皮建高, 孙锡良, 等, 1990.湖南省洞庭盆地第四纪地质研究报告.长沙:湖南省地质勘查局, 16-49. http://www.cnki.com.cn/Article/CJFDTOTAL-HNKC201104004.htm
      张建新, 申志军, 顾海滨, 等, 2007.洞庭湖区第四纪环境地球化学.北京:地质出版社, 28-44. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200603010.htm
      张人权, 梁杏, 张国梁, 等, 2001.洞庭湖区第四纪气候变化的初步探讨.地质科技情报, 20(2): 1-5. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200102000.htm
      张晓阳, 蔡述明, 孙顺才, 1994.全新世以来洞庭湖的演变.湖泊科学, 6(1): 13-21. doi: 10.18307/1994.0102
      赵举兴, 李长安, 许应石, 2014.洞庭盆地古沅江砾石层的沉积特征及沉积环境.地质科技情报, 33(1): 85-89. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201401014.htm
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