REVIEWS ON THE RESSEARCH OF LATE CENOZOIC GEOLOGY AND ENVIRONMENT OF THE YANGTZE RIVER DELTA AREA
-
摘要: 长江是我国最长的河流和世界最主要的大河之一，长江三角洲地区则是我国人口最为密集和经济最为发达的地区之一。因此，研究长江三角洲地区晚新生代地质与环境的特征与变化，特别是长江河口地区的河谷变迁与三角洲发育，对于该地区的国计民生，具有十分重要的意义。长江三角洲地区晚新生代地质与环境的科学调查研究，已经走过了整整的一个世纪。随着经济的发展和科技的进步，长江三角洲地区晚新生代地质与环境的研究也取得了重大的进展。本文从现代三角洲发育、末次盛冰期长江河谷的深切与充填作用及冰后期地层的沉积相变化，埋藏硬土层的分布、特征、成因及其古土壤学性质，三角洲地区晚第四纪时期的海侵地层层序与新近纪及早、中第四纪地层及其沉积环境，以及从三角洲钻孔的碎屑锆石、独居石年龄谱及沉积物成分和地球化学组成随时间的变化来推论长江贯通三峡的时间等方面所取得的进展和所存在的问题，按照研究时间的大体顺序和地层的新老次序进行了较详细的综述和简要评论。最后根据自己的认识和判断，概括了长江三角洲地区近一个世纪来研究工作所取得的进展和所存在的问题，并在此基础上提出了今后进一步工作的几点建议，希望能引起广大同仁及有关部门的注意，以期达到抛砖引玉的目的。Abstract: The Yangtze River is the longest river in China and one of the most main rivers in the world. The Yangtze River delta area is one of the most densely populated and economically developed areas in China. Therefore, studying characteristics and changes of Late Cenozoic geology and environment of the area is of very important significance for national welfare and the people's livelihood there. This kind of studies has had a whole century of history. With the development of economy and the progress of science and technology, some major progress has been made in this studies. In this paper we reviewed progress made on basis of data of such aspects as the modern development of the Yangtze River delta, incision and filling of the Yangtze River valleys during the latest pleniglacial age, changes of sedimentary facies during the post-glacial period, the distribution, characteristics and origin of buried hard earth layers, Late Quaternary transgressive sequences and Neogene and Early-Middle Quaternary stratigraphic units and sedimentary environments in the Yangtze River delta area, sedimentary compositions and geochemical analyses of delta sediments, and age spectrums of detrital zircon and monazite from borehole samples. Among the progress is the time of the Yangtze River breaking through the Three Gorges as an obstacle. At the same time some open questions were also pointed out in this paper. Then according to the reviews, we put forward several suggestions for the coming research to call researchers' attention to produce the effect of throwing away a brick in order to get a gem.
-
Key words:
- the Yangtze River delta /
- Late Cenozoic /
- geology /
- environment /
- review
-
图 1 长江三角洲及邻区地貌成因类型图[5]
Figure 1. Genelic type map of geomorphology of the Yangtze River Delta and its adjacent areas
图 2 长江三角洲全新世地层横剖面
Figure 2. Holocene stratigraphic cross section in the Yangtze River Delta
图 3 长江三角洲滨海平原发育过程图[7]
Figure 3. The development process of the coastal plain in the Yangtze River Delta
图 4 长江三角洲南部平原中全新世古地理图[9]
Figure 4. Middle holocene palaeogeography map of the southern plain of the Yangtze River Delta
图 5 苏北平原中部全新世海岸演化示意图[14]
Figure 5. Sketch map of Holocene coastal evolution in the middle part of the North Jiangsu Plain
图 6 建湖庆丰剖面全新世地层综合柱状图[13]
1—耕土；2—黏土；3—粉砂质黏土；4—黏土质粉砂；5—淤泥；6—细砂；7—贝壳缩聚；8—原位贝壳；9—腐木；10—潜穴；11—磁性地层柱；12—孢粉与微古取样点；13—14C取样点；14—孢粉带
Figure 6. Holocene comprehensive stratigraphic column of Qingfeng profile in Jianhu
图 7 里下河地区北部晚第四纪地层柱状对比图[14]
1—耕土或填土；2—粘土；3—淤泥；4—碳质淤泥；5—泥炭；6—亚粘土；7—亚砂土；8—砂；9—古土壤；10—贝壳层；11—原位贝壳或牡蛎壳；12—滨海相；13—海陆过渡相；14—陆相；15—风成相
Figure 7. Contrast figure of Late Quaternary stratigraphic column of the north part of the LiXia River area
图 11 南京长江四桥长江古河槽地质剖面示意图[18]
Figure 11. Sketch map of the ancient channel geological section in the forth Nanjing Yangtze river bridge
图 12 南京长江大桥长江古河槽地质剖面示意图[19]
Figure 12. Sketch map of the ancient channel geological section in the Nanjing Yangtze River Bridge
图 13 南京长江三桥附近长江古河槽地质剖面示意图[19]
Figure 13. Sketch map of the ancient channel geological section near the 3rd Nanjing Yangtze river bridge
图 14 上海面粉厂钻孔微体古生物分析综合柱状图[26]
Figure 14. Comprehensive column of micropaleontology analysis of Shanghai flour mill drilling
图 15 长江三角洲第四纪海侵范围图[29]
Figure 15. The Quaternary transgression range in Yangtze River Delta
图 16 太湖827孔中-上更新统有孔虫、海相介形虫种数、壳体数量统计[30]
Figure 16. Statistics of the middle-upper Pleistocene foraminifera、ostracods of marine species and the shells in the Taihu 827 drilling
图 18 磁性地层划分剖面磁化率对比图[35]
Figure 18. Comparison of magnetic susceptibility of magnetic stratigraphic sections
图 19 长江三角洲河口地区第四纪海陆相地层分布特征[36]
Figure 19. The distribution characteristics of the Quaternary marine-terrigenous facies strata in the Changjiang Estuary
图 20 浦东机场孔(Pd)第四系地层和地球化学微量元素及其比值、古地磁分布[36]
Figure 20. The Quaternary stratigraphy and Geochemical of trace elements and their ratios, paleomagnetic distribution in PD hole
图 21 长江三角洲DY03孔古地磁与磁化率测量结果[37]
Figure 21. Paleomagnetic and magnetic susceptibility of the DY03 hole in the Yangtze River Delta
图 22 长江三角洲DY03孔地层综合柱状图[37]
Figure 22. Comprehensive stratigraphic column of the DY03 hole in the Yangtze River Delta
图 24 长江三角洲南部5个钻孔的地层和孢粉绝对浓度(粒/g)分布[39]
Figure 24. Stratigraphy and absolute sporopollen concentration distribution of the 5 boreholes in the south of the Yangtze River delta
图 25 长江三角洲南部平原SG7孔新近纪-全新世孢粉图谱[39]
Figure 25. Neogene-Holocene Pollen spectrum of SG7 hole in southern plain of the Yangtze River Delta
图 26 江苏乐安镇—安亭—东海地层剖面图[40]
Figure 26. Stratigraphic section of Le'an town-Anting-Donghai in Jiangsu
图 27 太仓—宝应第四系地质结构剖面(NW向)[45]
Figure 27. Taicang-Baoying Quaternary geological structure profile (NW)
图 29 宝应钻孔沉积物常量元素含量随深度变化[48]
Figure 29. Variation of the content of constant elements in sediments with depth in Baoying borehole
图 30 兴化1#孔剖面地层、古地磁测定结果及其与标准极性柱的对比[51]
Figure 30. Profile stratum and paleomagnetic measurements of the 1# susceptibility with pore in Xinghua and the comparison with the standard pole column curve
图 31 质量磁化率与中值粒径和自然伽马测井曲线对比[51]
Figure 31. Comparison of mass median particle size and natural gamma logging
图 32 海安J9孔岩性剖面(a)及古地磁曲线(b)[56]
Figure 32. The lithologic section(a) and paleomagnetic curves (b) in Haian J9 hole
图 33 长江三角洲地区浅部硬土层分布略图[57]
1-基岩山区；2-下蜀粘土出露区；3-浅部硬土层缺失区；4-上部硬土层分布区；5-浅部硬土层顶板埋深等值线(米)；6-剖面线
Figure 33. Distribution map of shallow hard soil in the Yangtze River Delta
图 34 上海地区浅部硬土层分布图[57]
Figure 34. Distribution map of shallow hard soil in Shanghai area
图 35 杭嘉湖平原-上海地区浅部地层剖面[57]
Figure 35. The shallow stratigraphic profile of Hangjiahu Plain-Shanghai area
图 36 长江三角洲江北地区水文地质剖面图[57]
1—黏土、亚黏土；2—亚砂土；3—粉细砂、中细砂；4—含砾砂、砂砾石；5—基岩；6—矿化度界线及矿化度区阀值(克/升)；7—抽水钻孔：粗黑线为抽水试验段，左侧为矿化度(克/升)，右侧为涌水量(升/秒)和降深(米)
Figure 36. Hydrogeological profile of Jiangbei area in the Yangtze River Delta
图 37 西洋西潮流通道的地震剖面(a)及其解译图(b)[79]
Figure 37. Seismic profile (a) and its interpretation map of tidal currents
图 39 西洋西通道07SR01钻孔及地震地层单元与邻近研究钻孔的对比[79]
Figure 39. The strata and age of Wanggang tidal flat profile in Jiangsu Dafeng
图 41 长江三角洲南部地区晚更新世以来年代地层[82]
Figure 41. Chronostratigraphy since Late pleistocene in the southern region of the Yangtze River Delta
图 42 长江三角洲南部MFC孔综合剖面[82]
Figure 42. The comprehensive profile of MFC hole in the south of Yangtze River Delta
图 43 长江三角洲晚第四纪N-S剖面地质图[17]
Figure 43. The late Quaternary profile map of N-S section in the Yangtze River Delta
图 45 南黄海西部陆架浅地层剖面A4与钻孔对比[85]
Figure 45. Comparison between sub-bottom profile A4 and drilling in western continental shelf of the South Yellow Sea
图 46 南黄海各期三角洲分布范围[85]
Figure 46. The distribution range of the Delta in the South Yellow Sea at Each period
图 47 长江三角洲北翼第四系厚度等值线图[87]
Figure 47. Contour map of Quaternary thickness in the North Wing of Yangtze River Delta
图 48 长江三角洲现代构造运动强度图[88]
Figure 48. The intensity map of modern tectonic movement of the Yangtze River Delta
图 50 上海及邻区活动断裂和地震震中分布[90]
Figure 50. Distribution of active faults and earthquakes in Shanghai and its adjacent areas
图 52 长江三角洲晚新生代地层分布图[92]
Figure 52. Late Cenozoic stratigraphic distribution in the Yangtze River Delta
图 53 长江三角洲晚新生代地层和独居石测年[95]
Figure 53. The late Cenozoic stratum and monazite dating of the Yangtze river delta
图 54 长江三角洲晚新生代独居石年龄分布谱图[95]
Figure 54. Age distribution spectrum of the late Cenozoic monazites in the Yangtze river delta
图 55 PD钻孔岩性、143Nd/144Nd、CIA和REE分异参数比值的变化[97]
Figure 55. The lithology of PD borehole、143Nd/144Nd、CIA and variation of the REE differentiation parameter ratio
图 57 长江三角洲基岩埋深等值线和晚新生代沉积盆地分布[99]
Figure 57. Bedrock depth contour and the distribution of Late Cenozoic sedimentary basins in the Yangtze River Delta
图 61 XH-1孔磁化率与粒度分析结果[101]
Figure 61. Analysis of magnetic susceptibility and grain size of XH-1 hole
图 63 DY03孔主量与微量元素比值变化情况[102]
Figure 63. The change of the ratio of main and trace elements of DY03 hole
图 64 DY03孔碎屑锆石U-Pb年龄谱系随深度变化图[103]
Figure 64. The detrital zircon U-Pb age pedigree changes with depth in DY03 hole
图 65 长江流域太古宙—新生代(变)火成岩分布图[104]
Figure 65. The (Metamorphic) igneous rock distribution in Yangtze River Basin from Archaean to Cenozoic
图 66 长江三角洲第四系钻孔综合柱状图[105]
Figure 66. Quaternary borehole column of the Yangtze River Delta
图 67 长江三角洲第四纪控制性断裂和古长江改道示意图[105]
Figure 67. Schematic diagram of the Quaternary controlled faults and the ancient Yangtze River Diversion in the Yangtze River Delta
表 1 上海面粉厂全新世地层剖面特征简表[6]
Table 1. A brief table for the Holocene stratigraphic profile in Shanghai flour mill
下载: 导出CSV
表 4 上海东部地区第四纪地层综合表[26]
Table 4. Comprehensive table for Quaternary stratum in eastern Shanghai
下载: 导出CSV
表 5 上海面粉厂钻孔地层划分与海进层位表[26]
Table 5. Drilling stratigraphic division and transgressive table of Shanghai flour miu
时代 地层 井深(米) 海进旋回 大致厚度(米) 全新世 ${\text{Q}}_3^1$ 上海组 0~13.85 第Ⅰ海进层 25 ${\text{Q}}_3^2$ 13.85~17.4 ${\text{Q}}_3^3$ 17.4~25.4 晚更新世 ${\text{Q}}_3^3$ 南汇组 25.4~34.5 第Ⅰ陆相层 9 ${\text{Q}}_3^2$ 34.5~74.96 第Ⅱ海进层 40 ${\text{Q}}_3^1$ 川沙组 74.96~92 第Ⅱ陆相层 17 ${\text{Q}}_2^1$ 92~109.5 第Ⅲ海进层 18 早、中更新世 Q1-2 宝山群 109.5~133.2 第Ⅲ陆相层 23 133.2~160 第Ⅳ海进层 27 160~255.3 第Ⅳ陆相层 100
下载: 导出CSV
表 6 新近纪地层划分对比[46]
Table 6. Neogene stratigraphic division and correlation
年代地层 皖北平原 河北平原 南京附近 长江三角洲 统 阶(全球) 中国区域 上新统 Piacenzian3.60 Ma 麻则沟阶 常胜沟组 固安组 尖山组 干窑镇组 中新统 上 Messinian7.12 Ma 保德阶 辛集组 明化镇组 黄岗组 六合组 Tortonion11.2 Ma 中 Serravillian14.8 Ma 通古尔队 六合组 Langhian16.4 Ma 下 Burdigalian 山旺阶 固镇组 馆陶组 洞玄观组 洞玄观组 白龙港组 Aquitanian23.8 Ma 谢家阶 头铺组
下载: 导出CSV
表 7 上海及邻区活动断裂简表[90]
Table 7. A brief table for active faults in Shanghai and its adjacent areas
断裂方向 名称 图幅内长度/km 主要活动时代 断裂性(新构造期) 规模 北北东 郯庐断裂带 长100、宽20 燕山期—近期 右旋压扭 主干断裂 盐城—茅山—泾县断裂带 长400、宽4~20 燕山期—近期 右旋压扭 主干断裂 镇海—温州断裂带 长120 燕山期—第四纪 压扭 主干断裂 北东 苏北—南黄海盆地断裂系 长40~150不等 燕山期—第四纪 张扭 主干断裂和一般断裂 湖州—苏州断裂 长200 晚白垩纪—近期 张扭 主干断裂 肖山—球川断裂 长350、宽5.5~7.0 燕山期—近期 张扭 主干断裂 绍兴—江山断裂带 长280 元古代—第三纪 右旋张扭 主干断裂 东西 扬州—海安—拼茶河断裂 长240 晚白垩世—近期 张性 主干断裂 无锡—太仓—长江口断裂 长200 燕山期—近期 张性 主干断裂 昆山—嘉定断裂带 长60~80 白垩纪—近期 张性 主干断裂 昌化—杭州—杭州湾断裂 长300 燕山期—第四纪 张扭 主干断裂 北西 与郯庐断裂伴随的北西向断裂组 长30~80不等 第三纪—近期 左旋张扭或压扭 一般断裂 南京—溧阳断裂带 长140 晚白垩纪—近期 左旋张扭 一般断裂 太仓—奉贤断裂带 长140 晚白垩纪—近期 左旋张扭 一般断裂 南黄海盆地北西向断裂组 长30~70不等 第三纪—近期 张扭 一般断裂
下载: 导出CSV
表 8 DY03孔个层段常量元素平均含量[102]
Table 8. The average content of the major elements at each section in DY03 hole
地层 样品个数 元素平均含量/% Fe2O3 MnO TiO2 CaO K2O P2O5 SiO2 Al2O3 MgO Na2O Q4 9 5.73 0.09 0.85 2.48 2.67 0.12 64.47 12.82 2.83 1.37 Q3 22 3.98 0.07 0.64 2.62 2.22 0.11 70.60 9.51 1.79 1.54 Q2 16 4.14 0.07 0.67 3.93 2.25 0.11 67.45 9.71 2.02 1.31 Q1 23 3.80 0.06 0.59 3.52 2.08 0.09 71.97 8.46 1.64 1.16 N 20 3.49 0.06 0.49 1.45 2.35 0.06 75.26 8.35 1.08 0.92 基底 2 4.10 0.09 0.74 3.03 2.26 0.12 70.14 10.35 2.43 1.51
下载: 导出CSV
-
[1] Mosseman S. Delta of Yangtze[J]. Gepgr. Mag., 1877. [2] Von Heidenstan H. Report on Yangtze Estuary[R]. Whangpoo Conservancy Board, 1917. [3] Von Heidenstan H. The growth of Yangtze Delta[J]. Journal of the North China Branch Royal Asiatic Society, 1922, 58. https://www.sciencedirect.com/science/article/pii/S0304380010005235 [4] Ting V K. Geology of Yangtze Estuary below Wuhu[J]. Shanghai Harbour Investigation, 1919, (1): 1. http://www.sciencedirect.com/science/article/pii/002532279190155W [5] 陈吉余, 虞志英, 惲才兴.长江三角洲地貌发育[J].地理学报, 1959, 25(3): 201~220. http://www.cnki.com.cn/Article/CJFDTOTAL-DLXB195903004.htmCHEN Ji-yu, YU Zhi-ying, YUN Cai-xing. Landform development in the Yangtze River Delta[J]. Acta Geographica Sinica, 1959, 25(3): 201~220. http://www.cnki.com.cn/Article/CJFDTOTAL-DLXB195903004.htm [6] 王靖泰, 郭蓄民, 许世远, 等.全新世长江三角洲的发育[J].地质学报, 1981, 55(1): 67~81. http://cdmd.cnki.com.cn/Article/CDMD~10269~1015542986.htmWANG Jing-tai, GUO Xu-min, XU Shi-yuan, et al. Development of the Holocene Changjiang delta[J]. Acta Geologica Sinica, 1981, 55(1): 67~81. http://cdmd.cnki.com.cn/Article/CDMD~10269~1015542986.htm [7] 郭蓄民.长江河口地区晚更新世晚期以来沉积环境的变迁[J].地质科学, 1983, (4): 402~408. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX198304011.htmGUO Xu-min. Evolution of sedimentary environment of the Changjiang estuary area since the late stage of late Pleistocene[J]. Scientia Geologica Sinica, 1983(4): 402~408. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX198304011.htm [8] 李从先, 张桂甲.晚第四纪长江三角洲高分辨率地层学的初步研究.海洋地质与第四纪地[ http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ603.001.htmJ]. 1996, 16(3): 13~24. LI Cong-xian, ZHANG Gui-jia. A primary study on high-resolution sequence stratigraphy of late Quaternary in the Yangtze river delta area[J]. Marine Geology & Quaternary Geology, 1996, 16(3): 13~24. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ603.001.htm [9] 严钦尚, 洪雪晴.长江三角洲南部平原全新世海侵问题[J].海洋学报, 1987, 9(6): 744~762. http://www.cnki.com.cn/Article/CJFDTOTAL-SEAC198706009.htmYAN Qin-shang, HONG Xue-qing. The Holocene sea transgression in southern Changjiang delta plain[J]. Acta Oceanologica Sinica, 1987, 9(6): 744~762. http://www.cnki.com.cn/Article/CJFDTOTAL-SEAC198706009.htm [10] 严钦尚, 黄山.杭嘉湖平原全新世沉积环境的演变[J].地理学报, 1987, 42(1): 1~15. http://www.cnki.com.cn/Article/CJFDTOTAL-DLXB198701000.htmYAN Qin-shang, HUANG Shan. Evolution of Holocene sedimentary environment in the Hangzhou-Jiaxing-Huzhou plain[J]. Acta Geographica Sinica, 1987, 42(1): 1~15. http://www.cnki.com.cn/Article/CJFDTOTAL-DLXB198701000.htm [11] 赵希涛, 鲁刚毅, 王绍鸿, 等.江苏建湖庆丰剖面全新世地层及其对环境变迁与海面变化的反映[J].中国科学B辑, 1991, (9): 992~999. http://www.cnki.com.cn/Article/CJFDTOTAL-JBXK199109014.htmZHAO Xi-tao, LU Gang-yi, WANG Shao-hong, et al. The relation of the environmental variances and the sea-level changes with layers of Holocene in Jianhu, Jiangsu province[J]. Science in China(B), 1991, (9): 992~999. http://www.cnki.com.cn/Article/CJFDTOTAL-JBXK199109014.htm [12] 赵希涛, 李波, 鲁刚毅, 等.江苏阜宁西园全新世风暴沉积与海岸沙丘的发现及其意义[J].中国科学B辑, 1992, (9): 994~1001. http://www.cnki.com.cn/Article/CJFDTOTAL-JBXK199209014.htmZHAO Xi-tao, LI Bo, LU Gang-yi, et al. Holocene storm sediments and the significance of the coastal sand dune in Funing Xiyuan, Jiangsu[J]. Science in China(B), 1992, (9): 994~1001. http://www.cnki.com.cn/Article/CJFDTOTAL-JBXK199209014.htm [13] 赵希涛, 唐领余, 沈才明, 等.江苏建湖庆丰剖面全新世气候变迁和海面变化:中国沿海的一个典型实例[J].海洋学报, 1994, 16(1): 78~88.ZHAO Xi-tao, TANG Ling-yu, SHEN Cai-ming, et al. Holocene environment variance and the sea-level changes in layers of Jianhu-Qingfeng, Jiangsu[J]. Acta Oceanologica Sinica, 1994, 16(1): 78~88. [14] 赵希涛.中国海面变化[M].济南:山东科学技术出版社, 1996: 83~103.ZHAO Xi-tao. Sea level changes of China[M]. Jinan: Shandong Science and Technology Press, 1996: 83~103. [15] LI Cong-xian, WANG Ping, SUN HE-ping, et al. Late Quaternary incised-valley fill of the Yangtze delta (China): Its stratigraphic framework and evolution[J]. Sedimentary Geology, 2002, 152: 133~158. doi: 10.1016/S0037-0738(02)00066-0 [16] 李从先, 汪品先.长江晚第四纪河口地层学研究[M].北京:科学出版社, 1998: 1~222.LI Cong-xian, WANG Pin-xian. Estuarine stratigraphy in the late Quaternary of the Yangtze River[M]. Beijing: Science Press, 1998: 1~222. [17] 张家强, 陈庆强, 李从先.长江三角洲晚第四纪地层层序特征[J].同济大学学报:自然科学版, 1998, 26(4): 438~442. http://www.cnki.com.cn/Article/CJFDTOTAL-TJDZ199803030.htmZHANG Jia-qiang, CHEN Qing-qiang, LI Cong-xian. Characteristies of the Late Quaternary stratigraphic sequence in the Changjiang River delta area[J]. Journal of Tongji University, 1998, 26(4): 438~442. http://www.cnki.com.cn/Article/CJFDTOTAL-TJDZ199803030.htm [18] 曹光杰, 张学勤, 熊万英.长江河口段古河谷地层层序特征[J].地球科学与环境学报, 2006, 28(3): 1~5. http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX200603001.htmCAO Guang-jie, ZHANG Xue-qin, XIONG Wan-ying. Characteristics of post glacial incised-valley stratigraphic sequence in Yangtze river mouth area[J]. Journal of Earth Sciences and Environment, 2006, 28(3): 1~5. http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX200603001.htm [19] 曹光杰, 王建, 张学勤, 等.末次盛冰期南京段河槽特征及古流量[J].地理学报, 2009, 64(3): 331~338. doi: 10.11821/xb200903008CAO Guang-jie, WANG Jian, ZHANG Xue-qin, et al. Characteristics and runoff volume of the Yangtze River's paleo-valley at Nanjing reach in the last glacial maximum[J]. Acta Geographica Sinica, 2009, 64(3): 331~338. doi: 10.11821/xb200903008 [20] 曹光杰, 王建, 李彦彦.南京长江4桥附近长江古河谷沉积层序[J].地层学杂志, 2010, 34(4): 389~393. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ201004009.htmCAO Guang-jie, WANG Jian, LI Yan-yan. Sedimentary sequences of the Yangtze River paleo-valley near the No.4 Nanjing Yangtze River bridge since LGMA[J]. Journal of Stratigraphy, 2010, 34(4): 389~393. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ201004009.htm [21] 熊振, 侯康明, 李清河, 等.南京秦淮河流域汉府街第四纪标准钻孔及其地质意义[J].高校地质学报, 2010, 16(4): 498~508. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201004011.htmXIONG Zhen, HOU Kang-ming, LI Qing-he, et al. Quaternary standard drill hole and its geological significance in the Hanfu Street, the Qinhuai River basin, Nanjing[J]. Geological Journal of China Universities, 2010, 16(4): 498~508. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201004011.htm [22] 尚益.上海的第一孔钻孔[J].上海地质, 1981, (1): 82.SHANG Yi. The first drilling core in Shanghai[J]. Geology in Shanghai, 1981, (1): 82. [23] 克里赛G B.上海的地质(之二)[J].中国科学和艺术杂志, 1928, 8: 33, 9: 89. http://cdmd.cnki.com.cn/Article/CDMD~10280~1014166887.htmCressey G B. Geology of Shanghai[J]. Journal of Science and Art, 1928, 8: 33, 9: 89. http://cdmd.cnki.com.cn/Article/CDMD~10280~1014166887.htm [24] 《中国地层典》编委会.中国地层典:第四系[M].北京:地质出版社, 2000. Committee of Stratigraphical Lexicon of China. Stratigraphical Lexicon of China: Quaternary[M]. Beijing: Geological Publishing House, 2000. [25] 邱金波.上海晚新生代地层[J].上海地质, 1988, (4): 1~8. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD200901002.htmQIU Jin-bo. The division of late Neozoic strata in Shanghai[J]. Geology of Shanghai, 1988, (4): 1~8. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD200901002.htm [26] 闵秋宝, 汪品先.论上海地区的第四纪海进[J].同济大学学报, 1979, 7(2): 109~128. http://www.cnki.com.cn/Article/CJFDTOTAL-TJDZ197902009.htmMIN Qiu-bao, WANG Pin-xian. Quaternary transgressions in Shanghai region[J]. Journal of Tongji University, 1979, 7(2): 109~128. http://www.cnki.com.cn/Article/CJFDTOTAL-TJDZ197902009.htm [27] 汪品先, 闵秋宝, 卞云华, 等.我国东部第四纪海侵地层的初步研究[J].地质学报, 1981, (1): 1~13. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE198101000.htmWANG Pin-xian, MIN Qiu-bao, BIAN Yun-hua, et al. Strata of Quaternary transgressions in east China: A preliminary study[J]. Acta Geologica Sinica, 1981, (1): 1~13. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE198101000.htm [28] 赵松龄, 秦蕴珊.中国沿海近三十万年以来的海侵与海面变动[J].中国第四纪研究, 1985, 6(2): 97~103.ZHAO Song-ling, QIN Yun-shan. The sedimentary model and Quaternary transgressions in the continental shelf of China[J]. Quaternary Sciences, 1985, 6(2): 97~103. [29] 吴标云, 李从先.长江三角洲第四纪地层[M].北京:海洋出版社, 1987: 1~166.WU Biao-yun, LI Cong-xian. Quaternary strata in the Yangtze River Delta[M]. Beijing: Ocean Press, 1987: 1~166. [30] 杨怀仁, 王强, 杨达源.太湖827孔微体古生物研究及其环境变迁[J].海洋地质与第四纪地质, 1988, 8(2): 67~76. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198802008.htmYANG Huai-ren, WANG Qiang, YANG Da-yuan. Micropaleontology in the drilling core 827 and the paleoenvironment of the Taihu lake[J]. Marine Geology & Quaternary Geology, 1988, 8(2): 67~76. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198802008.htm [31] 陈义华.江苏太湖第四纪沉积环境[J].江苏地质, 2000, 24(2): 87~90. http://www.cnki.com.cn/Article/CJFDTOTAL-JSDZ200002003.htmCHEN Yi-hua. Quaternary sedimentary environment of Taihu lake[J]. Geology of Jiangsu, 2000, 24(2): 87~90. http://www.cnki.com.cn/Article/CJFDTOTAL-JSDZ200002003.htm [32] 钟石兰, 刘金陵, 李星学, 等.江苏太滆地区晚更新世以来古生物群及环境[J].微体古生物学报, 1999, 16(2): 167~180. http://www.cnki.com.cn/Article/CJFDTOTAL-WSGT902.002.htmZHONG Shi-lan, LIU Jin-ling, LI Xing-xue, et al. Preliminary study of biota and environments since late Pleistocene in the Tai-Ge area, southern Jiangsu province, China[J]. Acta Micropalaeontologica Sinica, 1999, 16(2): 167~180. http://www.cnki.com.cn/Article/CJFDTOTAL-WSGT902.002.htm [33] 周曙, 邹松梅, 刘志平, 等.江苏太湖平原北翼的第四纪孢粉与环境[J].微体古生物学报, 2001, 18(1): 70~75. http://www.cnki.com.cn/Article/CJFDTOTAL-WSGT200101009.htmZHOU Shu, ZOU Song-mei, LIU Zhi-ping, et al. Quaternary pollen analysis and paleo-environmental evolution in the northern part of Taihu plain, Jiangsu[J]. Acta Micropalaeontologica Sinica, 2001, 18(1): 70~75. http://www.cnki.com.cn/Article/CJFDTOTAL-WSGT200101009.htm [34] 蒋梦林, 刘志平.太湖平原西北部第四纪海侵[J].江苏地质, 2001, 25(2): 78~81. http://www.cnki.com.cn/Article/CJFDTOTAL-JSDZ200102005.htmJIANG Meng-lin, LIU Zhi-ping. The Quaternary marine transgression in the northwest of Taihu Lake plain[J]. Geology of Jiangsu, 2001, 25(2): 78~81. http://www.cnki.com.cn/Article/CJFDTOTAL-JSDZ200102005.htm [35] 王润华, 郭坤一, 于振江, 等.长江三角洲地区第四纪磁性地层学研究[J].地层学杂志, 2005, 29: 612~617. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ2005S1028.htmWANG Run-hua, GUO Kun-yi, YU Zhen-jiang, et al. Quaternary magneto-stratigraphy of the Yangtze delta area[J]. Journal of Stratigraphy, 2005, 29: 612~617. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ2005S1028.htm [36] 韦桃源, 陈中原, 魏子新, 等.长江河口区第四纪沉积物中的地球化学元素分布特征及其古环境意义[J].第四纪研究, 2006, 26(3): 397~405. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200603010.htmWEI Tao-yuan, CHEN Zhong-yuan, WEI Zi-xin, et al. The distribution of geochemical trace elements in the Quaternary sediments of the Changjiang river mouth and the paleoenvironmental implications[J]. Quaternary Sciences, 2006, 26(3): 397~405. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200603010.htm [37] 黄湘通, 郑洪波, 杨守业, 等.长江三角洲DY03孔磁性地层研究及其意义[J].海洋地质与第四纪地质, 2008, 28(6): 87~93. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200806015.htmHUANG Xiang-tong, ZHENG Hong-bo, YANG Shou-ye, et al. Magnetostratigraphy and its implications of core DY03 in the Yangtze river delta[J]. Marine Geology & Quaternary Geology, 2008, 28(6): 87~93. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200806015.htm [38] 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): 674~683. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200904011.htmZHAN Qing, WANG Zhang-hua, WANG Xin, et al. Grain-size characteristics and geomorphology evolution in late Cenozoic era sediments, Changjiang estuary[J]. Acta Sedimentologica Sinica, 2009, 27(4): 674~683. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200904011.htm [39] 周园军, 王张华, 李晓, 等.长江三角洲南部平原晚新生代特征孢粉分布及其对沉积地貌演变的意义[J].古地理学报, 2011, 13(3): 287~297. doi: 10.7605/gdlxb.2011.03.005ZHOU Yuan-jun, WANG Zhang-hua, LI Xiao, et al. Late Cenozoic diagnostic pollen-spore distribution in southern Yangtze Delta Plain: Depositional geomorphological implications[J]. Journal of Palaeogeography, 2011, 13(3): 287~297. doi: 10.7605/gdlxb.2011.03.005 [40] 祝晓彬, 吴吉春, 叶淑君, 等.长江三角洲(长江以南)地区深层地下水三维数值模拟[J].地理科学, 2005, 25(1): 68~73. http://www.cnki.com.cn/Article/CJFDTOTAL-DLKX20050100A.htmZHU Xiao-bin, WU Ji-chun, YE Shu-jun, et al. Three dimensional numerical simulation of groundwater resources in deep aquifers of the Changjiang delta (South of the Changjiang River)[J]. Scientia Geographica Sinica, 2005, 25(1): 68~73. http://www.cnki.com.cn/Article/CJFDTOTAL-DLKX20050100A.htm [41] 张平, 李向前, 潘明宝, 等.长江三角洲SZ04孔磁性地层研究及其意义[J].沉积学报, 2013, 6:1041~1049. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201306011.htmZHANG Ping, LI Xiang-qian, PAN Ming-bao, et al. Magnetostratigraphy of borehole SZ04 in the Yangtze River delta and its implications[J]. Acta Sedimentologica Sinica, 2013, 6: 1041~1049. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201306011.htm [42] 陈艇, 王张华, 强小科, 等.太湖平原WJ孔矿物磁学特征以及晚第四纪海侵事件[J].地球物理学报, 2013, (8):2748~2759. doi: 10.6038/cjg20130823CHEN Ting, WANG Zhang-hua, QIANG Xiao-ke, et al. Magnetic properties of minerals recorded by the borehole WJ and Late Quaternary transgressions in the Taihu plain, southern Yangtze Delta[J]. Chinese Journal of Geophysics, 2013, (8):2748~2759. doi: 10.6038/cjg20130823 [43] 蒋仁, 杨祝良, 于俊杰, 等.长江三角洲北翼兴化-通州地区第四纪地层划分及古环境分析[J].资源调查与环境, 2014, (4):263~269. http://www.cnki.com.cn/Article/CJFDTOTAL-HSDZ201404005.htmJIANG Ren, YANG Zhu-liang, YU Jun-jie, et al. Stratigraphic division of Quaternary strata and paleo-enviroment analysis for Xinghua-Tongzhou region in the north flank of the Yangze River delta[J]. Resources Survey and Environment, 2014, (4):263~269. http://www.cnki.com.cn/Article/CJFDTOTAL-HSDZ201404005.htm [44] 蒋仁, 于俊杰, 劳金秀, 等.长江三角洲北翼ZKA4钻孔剖面第四纪磁性地层特征及其意义[J].中国地质调查, 2015, (7):30~34. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDC201507006.htmJIANG Ren, YU Jun-jie, LAO Jin-xiu, et al. Characteristics and implications of the Quaternary magnetostratigraphy in borehole ZKA4 from the northern flank of Yangtze River Delta[J]. Geological Survey of China, 2015, 0(7): 30~34. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDC201507006.htm [45] 苗巧银, 宗开红, 陈火根, 等.长江三角洲(江苏)地区第四纪地层沉积分区及沉积特征[J].上海国土资源, 2016, (2):51~56, 64. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD201602013.htmMIAO Qiao-yin, ZONG Kai-hong, CHEN Huo-gen, et al. Sedimentary division and characteristics of the Quaternary strata in the Yangtze River Delta (Jiangsu) region[J]. Shanghai Land & Resources, 2016, (2):51~56, 64. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD201602013.htm [46] 于振江, 张于平, 王润华, 等.长江三角洲(江南)地区新近纪地层划分及时代讨论[J].地层学杂志, 2004, 28(3): 257~264. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ200403010.htmYU Zhen-jiang, ZHANG Yu-ping, WANG Run-hua, et al. The division and age of the Neogene strata in the Yangtze delta area[J]. Journal of Stratigraphy, 2004, 28(3): 257~264. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ200403010.htm [47] 王颖, 张振克, 朱大奎, 等.河海交互作用与苏北平原成因[J].第四纪研究, 2006, 26(3): 301~320. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200603000.htmWANG Ying, ZHANG Zhen-ke, ZHU Da-kui, et al. River-sea interaction and the north Jiangsu plain formation[J]. Quaternary Sciences, 2006, 26(3): 301~320. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200603000.htm [48] 杨兢红, 王颖, 张振克, 等.苏北平原2.58 Ma以来的海陆环境演变历史——宝应钻孔沉积物的常量元素记录[J].第四纪研究, 2006, 26(3): 343~351. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200603004.htmYANG Jing-hong, WANG Ying, ZHANG Zhen-ke, et al. Major element records of land-sea interaction and evolution in the past 2.58 Ma from the Baoying borehole sediments, northern Jiangsu plain, China[J]. Quaternary Sciences, 2006, 26(3): 343~351. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200603004.htm [49] 杨兢红, 王颖, 张振克, 等.宝应钻孔沉积物微量元素地球化学特征及沉积环境探讨[J].第四纪研究, 2007, 27(5): 735~749. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200705017.htmYANG Jing-hong, WANG Ying, ZHANG Zhen-ke, et al. Geochemical characteristics of trace elements in Baoying borehole sediments and their implications for depositional environments[J]. Quaternary Sciences, 2007, 27(5): 735~749. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200705017.htm [50] 杨得志, 张振克, 毛龙江, 等.苏北By1孔粒度特征、含水层分布与苏北平原地下水资源保护[J].第四纪研究, 2010, 30(1): 159~166. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ201001016.htmYANG De-zhi, ZHANG Zhen-ke, MAO Long-jiang, et al. Grain size characteristics, aquifer distribution of core By1 and ground water protection in northern Jiangsu province[J]. Quaternary Sciences, 2010, 30(1): 159~166. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ201001016.htm [51] 舒强, 卫艳, 李吉均, 等.苏北盆地兴化1#钻孔沉积物磁化率特征及其气候环境意义[J].地质科技情报, 2005, 24(4): 31~36. http://cdmd.cnki.com.cn/Article/CDMD~10319~2007108234.htmSHU Qiang, WEI Yan, LI Ji-jun, et al. Characteristics and paleoclimatic and paleoenvironmental implication of sedimentary susceptibility of Xinghua[J]. Geological Science and Technology Information, 2005, 24(4): 31~36. http://cdmd.cnki.com.cn/Article/CDMD~10319~2007108234.htm [52] 卫艳, 舒强, 陈晔.苏北盆地兴化1#钻孔的沉积物粒度特征及其古环境意义[J].南京师大学报:自然科学版, 2005, 28(2): 101~107. http://cdmd.cnki.com.cn/Article/CDMD~10319~2007108234.htmWEI Yan, SHU Qiang, CHEN Ye. Grain size characteristics and their Paleo environmental significance of Xinghua 1# Core sediments in northern Jiangsu Basin, China[J]. Journal of Nanjing Normal University: Natural Science Edition, 2005, 28(2): 101~107. http://cdmd.cnki.com.cn/Article/CDMD~10319~2007108234.htm [53] 舒强, 李吉均, 赵志军, 等.苏北盆地XH~1钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究[J].沉积学报, 2006, 24(2): 276~281. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200602016.htmSHU Qiang, LI Ji-jun ZHAO Zhi-jun, et al. A correlation between magnetic susceptibility and the content of different grain sizes of XH~1# Core in north Jiangsu Basin and its significance[J]. Acta Sedimentologica Sinica, 2006, 24(2): 276~281. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200602016.htm [54] 朱芸, 陈晔, 舒强, 等.苏北盆地XH1钻孔中更新世以来的彩度指标记录及其气候环境变化[J].海洋地质与第四纪地质, 2007, 27(2): 23~31. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200702004.htmZHU Yun, CHEN Ye, SHU Qiang, et al. Chroma index record of core XH1 at northern Jiangsu basin and the climate since midpleistocene[J]. Marine Geology & Quaternary Geology, 2007, 27(2): 23~31. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200702004.htm [55] 舒强, 萧家仪, 赵志军, 等.苏北盆地XH~1钻孔0.78Ma以来的气候环境变化记录[J].地层学杂志, 2010, 27(2): 27~34. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ201001007.htmSHU Qiang, XIAO Jia-yi, ZHAO Zhi-jun, et al. Environmental records in XH~1 core in northern Jiangsu basin since about 780 kaBP[J]. Journal of Stratigraphy, 2010, 27(2): 27~34. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ201001007.htm [56] 缪卫东, 李世杰, 王润华.长江三角洲北翼J9孔岩芯沉积特征及地层初步划分[J].第四纪研究, 2009, 29(1): 126~134.MIU Wei-dong, LI Shi-jie, WANG Run-hua. Preliminary study on sedimentary characteristics and stratum division of J9 core in the north wing of the Yangtze river delta[J]. Quaternary Sciences, 2009, 29(1): 126~134. [57] 冯铭璋.关于长江三角洲地区浅部硬土层[J].上海地质, 1980, (2): 44~57. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD198002006.htmFENG Ming-zhang. On the shallow hard soil layer in the Yangtze River delta area[J]. Shanghai Geology, 1980, (2): 44~57. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD198002006.htm [58] 郑祥民, 严钦尚, 郭蓄民.长江三角洲现代沉积[M].上海:华东师范大学出版社, 1987: 76~91.ZHENG Xiang-min, YAN Qin-shang, GUO Xu-min. Modern sediments in the Yangtze River Delta[M]. Shanghai: Huadong Normal University Press, 1987: 76~91. [59] 郑祥民, 俞立中.上海地区晚更新世晚期暗绿色硬土层风积黄土成因说[J].上海地质, 1991, (2): 13~21. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD199102002.htmZHENG Xiang-min, YU Li-zhong. Aeolian deposit genesis of dark-green hard clay as Holocene basement strata in Shanghai region[J]. Shanghai Geology, 1991, (2): 13~21. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD199102002.htm [60] 郑祥民, 严钦尚.末次冰期苏北平原和东延海区的风尘黄土沉积[J].第四纪研究, 1995, (3): 258~266. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ503.007.htmZHENG Xiang-min, YAN Qin-shang. Aeolian loess deposition during the last glacial period in the northern jiangsu plain of the Yangtze delta and western areas of the Yellow Sea and the East China Sea[J]. Quaternary Sciences, 1995, (3): 258~266. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ503.007.htm [61] 郑祥民, 彭家亮, 郑玉龙.东海海底末次冰期埋藏风成黄土地层初步研究[J].海洋地质与第四纪地质, 1993, 13(3): 49~56. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ199303005.htmZHENG Xiang-min, PENG Jia-liang, ZHENG Yu-long. On the buried aeolian loess strata of the last glacial period in the floor of the East China Sea[J]. Marine Geology & Quaternary Geology, 1993, 13(3): 49~56. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ199303005.htm [62] 陈报章, 李从先, 业治铮.长江三角洲北翼全新统底界和"硬黏土层"的讨论[J].海洋地质与第四纪地质, 1991, 11(2): 37~46. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ199102006.htmCHEN Bao-zhang, LI Cong-xian, YE Zhi-jing. Holocene bottom boundary and "hard clay band" in the northern flank of the Changjiang River delta[J]. Marine Geology & Quaternary Geology, 1991, 11(2): 37~46. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ199102006.htm [63] 李萍, 孙和平.长江三角洲地区晚更新世地层中的古土壤特征[J].上海地质, 1991, (1): 16~24. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD199101002.htmLI Ping, SUN He-ping. The characteristic of paleo-soil in the late-Pleistocene strata in the Changjiang delta[J]. Shanghai Geology, 1991, (1): 16~24. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD199101002.htm [64] 刘宝柱, 李从先, 业治铮, 等.沉积磁组构在长江三角洲晚第四纪古土壤研究中的应用[J].海洋地质与第四纪地质, 1994, 14(2): 55~62. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ402.005.htmLIU Bao-zhu, LI Cong-xian, YE Zhi-zheng, et al. Applications of magnetic fabrics to the studies of late Quaternary paleosols in the Changjiang River delta area[J]. Marine Geology & Quaternary Geology, 1994, 14(2):55~62. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ402.005.htm [65] 刘宝柱, 李从先, 业治铮.长江三角洲地区晚第四纪古土壤中植物硅酸体及其古环境意义[J].海洋地质与第四纪地质, 1995, 15(2): 17~24. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ502.002.htmLIU Bao-zhu, LI Cong-xian, YE Zhi-zheng. Phytolith and its paleo environmental significance in the studies of late Quaternary paleosols in the Yangtze delta area[J]. Marine Geology & Quaternary Geology, 1995, 15(2): 17~24. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ502.002.htm [66] 刘宝柱, 李从先, 业治铮.长江三角洲地区晚第四纪古土壤地球化学特征[J].青岛海洋大学学报, 1998, 28(1): 129~134. http://www.cnki.com.cn/Article/CJFDTOTAL-QDHY801.022.htmLIU Bao-zhu, LI Cong-xian, YE Zhi-zheng. Geochemical characteristics of the late Quaternary paleosols in the Yangtze River delta area[J]. Periodical of Ocean University of China, 1998, 28(1): 129~134. http://www.cnki.com.cn/Article/CJFDTOTAL-QDHY801.022.htm [67] 陈中原, 许丗远.尼罗河与长江三角洲晚更新世末期硬土层特征及其成因对比研究[J].第四纪研究, 1996, (2): 168~173. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ602.008.htmCHEN Zhong-yuan, XU Shi-yuan. Comparative study of the late Pleistocene Nile and Yangtze stiff muds: Sediment and origin[J]. Quaternary Sciences, 1996, (2): 168~173. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ602.008.htm [68] 陈庆强, 李从先.长江三角洲地区晚第四纪古土壤与古环境初探[J].沉积学报, 1995, 13: 79~87. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB5S1.009.htmCHEN Qing-qiang, LI Cong-xian. Preliminary study on late Quaternary paleosols and paleo environments of the Yangtze delta[J]. Acta Sedimentologica Sinica, 1995, 13: 79~87. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB5S1.009.htm [69] 陈庆强, 李从先.长江三角洲地区晚第四纪古土壤发育的阶段性[J].科学通报, 1998, 43(23): 2557~2559. doi: 10.3321/j.issn:0023-074X.1998.23.023CHEN Qing-qiang, LI Cong-xian. The stage of the late Quaternary Paleosols in the Yangtze River delta area[J]. Chinese Science Bulletin, 1998, 43(23): 2557~2559. doi: 10.3321/j.issn:0023-074X.1998.23.023 [70] 邓兵, 吴国瑄, 李从先.长江三角洲地区第一古土壤层及其古气候记录[J].海洋地质与第四纪地质, 1999, 19(3): 29~37. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ903.004.htmDENG Bing, WU Guo-xuan, LI Cong-xian. Paleoclimate recorded in the first layer of paleosol in Yangtze delta area[J]. Marine Geology & Quaternary Geology, 1999, 19(3): 29~37. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ903.004.htm [71] 邓兵, 吴国瑄, 李从先.长江三角洲晚第四纪古土壤的古环境及古气候信息[J].海洋地质与第四纪地质, 2003, 23(2): 1~7. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200302001.htmDENG Bing, WU Guo-xuan, LI Cong-xian. Paleoenvironment and paleoclimate characteristics of late Quaternary paleosol in the Yangtze River delta area[J]. Marine Geology & Quaternary Geology, 2003, 23(2): 1~7. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200302001.htm [72] 邓兵, 李从先, 张经, 等.长江三角洲古土壤发育与晚更新世末海平面变化的耦合关系[J].第四纪研究, 2004, 24(2): 222~230. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200402014.htmDENG Bing, LI Cong-xian, ZHANG Jing, et al. Correlation of paleosol development in the Changjiang delta with sea level fluctuations in the late Pleistocene[J]. Quaternary Sciences, 2004, 24(2): 222~230. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200402014.htm [73] 覃军干, 吴国瑄, 邓兵, 等.长江三角洲第一古土壤层的孢粉、藻类及其古环境意义[J].科学通报. 2002, 47(17): 1347~1350. doi: 10.3321/j.issn:0023-074X.2002.17.015QIN Jun-gan, WU Guo-xuan, DENG Bing, et al. The first ancient soil layer of pollen and algae and its paleoenvironmental significance in the Yangtze River delta area[J]. Chinese Science Bulletin, 2002, 47(17): 1347~1350. doi: 10.3321/j.issn:0023-074X.2002.17.015 [74] 邱金波.上海市浅部数层硬土的沉积环境、时代及划分对比[J].上海地质, 2005, 93: 4~9. doi: 10.3969/j.issn.2095~1329.2005.01.002QIU Jin-bo. A few stiff clay layer in the shallow of Shanghai municipality[J]. Shanghai Geology, 2005, 93: 4~9. doi: 10.3969/j.issn.2095~1329.2005.01.002 [75] 金秉福, 张云吉, 宋键.长江三角洲第一硬土层中微结核的矿物化学特征及其成因[J].海洋地质与第四纪地质, 2007, 27(3): 9~15. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200703001.htmJIN Bing-fu, ZHANG Yun-ji, SONG Jian. Characteristics of mineral chemistry and formation of the micro-nodules in the first stiff clay layer in the Yangtze river delta[J]. Marine Geology & Quaternary Geology, 2007, 27(3):9~15. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200703001.htm [76] 施雅风, 于革. 30~40 kaBP中国暖湿气候和海侵的特征与成因探讨[J].第四纪研究, 2003, 23(1): 1~11. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200301000.htmSHI Ya-feng, YU Ge. Warm-humid climate and transgressions during 40~30 kaBP and their potential mechanisms[J]. Quaternary Sciences, 2003, 23(1): 1~11. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200301000.htm [77] 杨达源, 陈可锋, 舒肖明.深海氧同位素第3阶段晚期长江三角洲古环境初步研究[J].第四纪研究, 2004, 24(5): 525~530. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200405007.htmYANG Da-yuan, CHEN Ke-feng, SHU Xiao-ming. A preliminary study on the paleoenvironment during MIS 3 in the Changjiang delta region[J]. Quaternary Sciences, 2004, 24(5): 525~530. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200405007.htm [78] 王建, 沙润, 汪永进, 等.江苏中部粉砂淤泥质滩岸剖面所揭示的滩岸发育过程与环境演变[J].沉积学报, 1997, 15: 51~56. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB1997S1011.htmWANG Jian, SHA Run, WANG Yong-jin, et al. Coastal development and environmental evolution in central part of Jiangsu province derived from a long drilling section[J]. Acta Sedimentologica Sinica, 1997, 15: 51~56. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB1997S1011.htm [79] 夏非, 殷勇, 王强, 等. MIS 3晚期以来江苏中部海岸的层序地层[J].地质学报, 2012, 86(10): 1696~1712. doi: 10.3969/j.issn.0001~5717.2012.10.009XIA Fei, YIN Yong, WANG Qiang, et al. Sequence stratigraphy of the central part of north Jiangsu coasts since late MIS 3, eastern China[J]. Acta Geologica Sinica, 2012, 86(10): 1696~1712. doi: 10.3969/j.issn.0001~5717.2012.10.009 [80] Skene K I, Piper D J W, Aksu A E, et al. Evaluation of the global oxygen isotope curve as a proxy for Quaternary sea level by modeling of delta progradation[J]. Journal of Sedimentary Research, 1998, 68: 1077~1092. doi: 10.2110/jsr.68.1077 [81] 张振克, 谢丽, 张云峰, 等.苏北平原MIS 3阶段海侵事件的沉积记录[J].第四纪研究, 2010, 30(5): 883~891. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ201005007.htmZHANG Zhen-ke, XIE Li, ZHANG Yun-feng, et al. Sedimentary records of the MIS 3 transgression event in the north Jiangsu plain China[J]. Quaternary Sciences, 2010, 30(5): 883~891. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ201005007.htm [82] 王张华, 邱金波, 冉莉华, 等.长江三角洲地区晚更新世年代地层和海水进退[J].海洋地质与第四纪地质, 2004, 24(4): 1~8. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200404000.htmWANG Zhang-hua, QIU Jin-bo, RAN Li-hua, et al. Chronostratigraphy and transgression/regression during late Pleistocene in the southern Changjiang (Yangtze) River delta plain[J]. Marine Geology & Quaternary Geology, 2004, 24(4): 1~8. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200404000.htm [83] 王颖, 邹欣庆, 殷勇, 等.河海交互作用与黄东海古扬子大三角洲体系研究[J].第四纪研究, 2012, 32(6): 1055~1064. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ201206003.htmWANG Ying, ZOU Xin-qing, YIN Yong, et al. Study on river-sea interaction and formation of paleo-Yangtze grand delta system in the area of south Yellow Sea and East China Sea[J]. Quaternary Sciences, 2012, 32(6): 1055~1064. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ201206003.htm [84] 史照良.江苏省地图集[M].北京:中国地图出版社, 2004: 8~9.SHI Zhao-liang. Maps of Jiangsu Province[M]. Beijing: China Map Publishing House, 2004: 8~9. [85] 陶倩倩, 刘宝华, 李西双, 等.晚更新世南黄海西部陆架的古长江三角洲[J].海洋地质与第四纪地质, 2009, 29(2): 15~24. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200902006.htmTAO Qian-qian, LIU Bao-hua, LI Xi-shuang, et al. Late Pleistocene evolution of the paleo Yangtze delta in the South Yellow Sea[J]. Marine Geology & Quaternary Geology, 2009, 29(2): 15~24. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200902006.htm [86] 杨子赓, 林和茂, 张光威. 黄海陆架第四纪地层[C]//杨子赓, 林和茂. 中国第四纪地层与国际对比[M]. 北京: 科学出版社, 1996: 31~55.YANG Zi-geng, LIN He-mao, ZHANG Guang-wei. Quaternary stratigraphy in the shelf of the Yellow Sea[C]//YANG Zi-geng, LIN He-mao. Comparison of Quaternary strata in China and international[M]. Beijing: Science Press, 1996: 31~55. [87] 孙顺才.长江三角洲全新世沉积特征[J].海洋学报, 1981, 3(1): 87~101. http://www.cnki.com.cn/Article/CJFDTOTAL-SEAC198101008.htmSUN Shun-cai. Deltaic sediments of the Changjiang delta and its characteristics[J]. Acta Oceanologica Sinica, 1981, 3(1): 87~101. http://www.cnki.com.cn/Article/CJFDTOTAL-SEAC198101008.htm [88] 虞志英. 长江三角洲新构造运动[C]//陈吉余, 沈焕庭. 长江河口动力学. 上海: 上海科技出版社, 19~30.YU Zhi-ying. Neotectonics of the Yangtze River Delta[C]//CHEN Ji-yu, SHEN Huan-ting. Dynamics of the Yangtze River Estuary. Shanghai: Shanghai Science and Tecnology Press, 19~30. [89] 顾澎涛, 程之牧.也谈上海地区的断裂构造系统[J].上海地质, 1990, (4): 1~6. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD199004000.htmGU Peng-tao, CHENG Zhi-mu. On fracture tectonic system in Shanghai area[J]. Shanghai Geology, 1990, (4): 1~6. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD199004000.htm [90] 朱履熹, 顾志文.上海及邻区活动断裂和地震震中分布图[J].华东师范大学学报:自然科学版, 1994, (2): 77~83.ZHU Lü-xi, GU Zhi-wen. Discussion to the background of the seismogeology and the basic earthquake intensity in Shanghai and its vicinity[J]. Journal of East China Normal University: Natural Science, 1994, (2): 77~83. [91] 顾志文.试论上海及邻区晚新生代沉积特征与断裂的关系[J].华东师范大学学报:自然科学版, 1997, (2): 68~75. http://www.cnki.com.cn/Article/CJFDTOTAL-HDSZ199702010.htmGU Zhi-wen. On the relationship between sedimentary feature and faulted structure of upper Cenozoic Group in Shanghai and its adjacent regions[J]. Journal of East China Normal University: Natural Science, 1997, (2): 68~75. http://www.cnki.com.cn/Article/CJFDTOTAL-HDSZ199702010.htm [92] 陈中原.长江三角洲之沉降[J].火山地质与矿产, 2001, (2): 95~101. http://www.cnki.com.cn/Article/CJFDTOTAL-HSDZ200102003.htmCHEN Zhong-yuan. Yangtze delta subsidence[J]. Volcanology & Mineral Resources, 2001, (2): 95~101. http://www.cnki.com.cn/Article/CJFDTOTAL-HSDZ200102003.htm [93] Gibbard P, Cohen K M. Global chronostratigraphic correlation table for the last 2.7 million years[J]. Episodes, 2008, 31: 243~247. https://dspace.library.uu.nl/handle/1874/179921 [94] 杨守业, 蔡进功, 李从先, 等.黄河贯通时间的新探索[J].海洋地质与第四纪地质, 2001, 21(2): 15~20. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200102003.htmYANG Shou-ye, CAI Jin-gong, LI Cong-xian, et al. New discussion about the run-through time of the Yellow River[J]. Marine Geology & Quaternary Geology, 2001, 21(2): 15~20. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200102003.htm [95] 范代读, 李从先, K Yokoyama, 等.长江三角洲晚新生代地层独居石年龄谱与长江贯通时间研究[J].中国科学D辑, 2004, 34(11): 1015~1022. doi: 10.3321/j.issn:1006~9267.2004.11.003FAN Dai-du, LI Cong-xian, K Yokoyama, et al. Monazite age spectrum time study in the Yangtze River Delta in the late Cenozoic strata[J]. Science in China(D), 2004, 34(11): 1015~1022. doi: 10.3321/j.issn:1006~9267.2004.11.003 [96] 范代读, 李从先.长江贯通时限研究进展[J].海洋地质与第四纪地质, 2007, 27(2): 121~131. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200702021.htmFAN Dai-du, LI Cong-xian. Reviews on researches of timing of the Yangtze draining the Tibetan Plateau to the East China Sea[J]. Marine Geology & Quaternary Geology, 2007, 27(2): 121~131. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200702021.htm [97] 杨守业, 韦刚健, 夏小平, 等.长江口晚新生代沉积物的物源研究: REE和Nd同位素制约[J].第四纪研究, 2007, 27(3): 339~346. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200703004.htmYANG Shou-ye, WEI Gang-jian, XIA Xiao-ping, et al. Provenance study of the late Cenozoic sediments in the Changjiang delta: REE and ND isotopic constraints[J]. Quaternary Sciences, 2007, 27(3): 339~346. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200703004.htm [98] 陈静, 王哲, 王张华, 等.长江三角洲东西部晚新生代地层中重矿物差异及其物源意义[J].第四纪研究, 2007, 27(5): 700~708. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200705013.htmCHEN Jing, WANG Zhe, WANG Zhang-hua, et al. Heavy mineral distribution and its provenance implication in late Cenozoic sediments in western and eastern area of the Changjiang River delta[J]. Quaternary Sciences, 2007, 27(5): 700~708. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200705013.htm [99] 王张华, 张丹, 李晓, 等.长江三角洲晚新生代沉积物磁性特征和磁性矿物及其指示意义[J].中国地质, 2008, 35(4): 670~682. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200804012.htmWANG Zhang-hua, ZHANG Dan, LI Xiao, et al. Magnetic properties and relevant minerals of late Cenozoic sediments in the Yangtze River delta and their implications[J]. Geology in China, 2008, 35(4): 670~682. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200804012.htm [100] 张丹, 王张华, 卫巍, 等.长江三角洲地区晚新生代沉积物磁学特征及其物源指示意义[J].第四纪研究, 2009, 29(2): 308~317. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200902022.htmZHANG Dan, WANG Zhang-hua, WEI wei, et al. Rock magnetic properties and source indications of late Cenozoic sediments in Yangtze delta area[J]. Quaternary Sciences, 2009, 29(2): 308~317. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200902022.htm [101] 舒强, 张茂恒, 赵志军, 等.苏北盆地XH~1钻孔晚新生代沉积记录特征及其与长江贯通时间的关联[J].地层学杂志, 2008, 32(3): 308~314. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ200803012.htmSHU Qiang, ZHANG Mao-heng, ZHAO Zhi-jun, et al. Sedimentary record from the XH~1 core in north Jiangsu basin and its implication on the Yangtze River run-through time[J]. Journal of Stratigraphy, 2008, 32(3): 308~314. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ200803012.htm [102] 黄湘通, 郑洪波, 杨守业, 等.长江三角洲DY03孔沉积物元素地球化学及其物源示踪意义[J].第四纪研究, 2009, 29: 299~307. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200902021.htmHUANG Xiang-tong, ZHENG Hong-bo, YANG Shou-ye, et al. Investigation of sedimentary geochemistry of core DY03 in the Yangtze delta: Implications to tracing provenance[J]. Quaternary Sciences, 2009, 29: 299~307. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200902021.htm [103] 贾军涛, 郑洪波, 黄湘通, 等.长江三角洲晚新生代沉积物碎屑锆石U-Pb年龄及其对长江贯通的指示[J].科学通报, 2010, 55(4/5): 350~358. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB2010Z1009.htmJIA Jun-tao, ZHENG Hong-bo, HUANG Xiang-tong, et al. Detrital zircon U-Pb ages of late Cenozoic sediments from the Yangtze delta: Implication for the evolution of the Yangtze River[J]. Chinese Science Bulletin, 2010, 55(4/5): 350~358. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB2010Z1009.htm [104] 贾军涛, 郑洪波, 杨守业.长江流域岩体的时空分布与碎屑锆石物源示踪[J].同济大学学报:自然科学版, 2010, 38(9): 1375~1380. http://www.cnki.com.cn/Article/CJFDTOTAL-TJDZ201009025.htmJIA Jun-tao, ZHENG Hong-bo, YANG Shou-ye. Rock types in Yangtze drainage and their implications for Zircon U-Pb provenance study of Yangtze sediments[J]. Journal of Tongji University, 2010, 38(9): 1375~1380. http://www.cnki.com.cn/Article/CJFDTOTAL-TJDZ201009025.htm [105] 黎兵, 魏子新, 李晓, 等.长江三角洲第四纪沉积记录与古环境响应[J].第四纪研究, 2011, 31(2): 316~328. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ201102013.htmLI Bing, WEI Zi-xin, LI Xiao, et al. Records from Quaternary sediment and palaeo-environment in the Yangtze river delta[J]. Quaternary Sciences, 2011, 31(2): 316~328. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ201102013.htm [106] 杨守业, 蒋少涌, 凌洪飞, 等.长江河流沉积物Sr-Nd同位素组成与物源示踪[J].中国科学D辑:地球科学, 2007, 37(5): 682~690. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200705012.htmYANG Shou-ye, JIANG Shao-yong, LING Hong-fei, et al. Sr-Nd isotopic composition and provenance tracing in the sediments of the Yangtze River[J]. Science in China(D), 2007, 37(5): 682~690. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200705012.htm [107] 王中波, 杨守业, 王汝成, 等.长江河流沉积物磁铁矿化学组成及其物源示踪[J].地球化学, 2007, 36(2): 176~184. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200702007.htmWANG Zhong-bo, YANG Shou-ye, WANG Ru-cheng, et al. Magnetite compositions of Changjiang River sediments and their tracing implications[J]. Geochimica, 2007, 36(2): 176~184. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200702007.htm [108] 张玉芬, 李长安, 王秋良, 等.江汉平原沉积物磁学特征及对长江三峡贯通的指示[J].科学通报, 2008, 53(5): 577~582. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200805014.htmZHANG Yu-fen, LI Chang-an, WANG Qiu-liang, et al. Magnetic characteristics of sediments in Jianghan Plain and its indication to the forming of the Three Gorges[J]. Chinese Science Bulletin, 2008, 53(5): 577~582. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200805014.htm [109] 何梦颖, 郑洪波, 黄湘通, 等.长江流域粘土矿物组合特征及物源指示意义[J].沉积学报, 2011, 29(3): 544~551.HE Meng-ying, ZHENG Hong-bo, HUANG Xiang-tong, et al. Characteristics of clay mineral assemblage in the Yangtze River Basin and their implications for provenance[J]. Acta Sedimentologica Sinica, 2011, 29(3): 544~551. [110] 范代读, 王扬扬, 吴伊婧.长江沉积物源示踪研究进展[J].地球科学进展, 2012, 27(5): 515~528. http://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ201205003.htmFAN Dai-du, WANG Yang-yang, WU Yi-jing. Advances in provenance studies of Changjiang Riverine sediments[J]. Advances in Earth Science, 2012, 27(5): 515~528. http://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ201205003.htm [111] 罗超, 郑妍, 郑洪波, 等.长江流域悬浮物磁性特征及其物源指示意义[J].第四纪研究, 2013, 33(4): 684~696. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ201304006.htmLUO Chao, ZHENG Yan, ZHENG Hong-bo, et al. Magnetic properties of suspended sediment in the Yangtze river and its provenance implications[J]. Quaternary Sciences, 2013, 33(4): 684~696. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ201304006.htm -
下载:
计量
- 文章访问数: 1043
- HTML全文浏览量: 287
- PDF下载量: 121
- 被引次数: 0
