Research progress on distribution of Quaternary buried paleo-Yangtze River channels in the North Jiangsu-western South Yellow Sea

CHEN Yingying; XIA Fei; ZHANG Zhenke; XU Qinmian; CHEN Shiyue

doi:10.16562/j.cnki.0256-1492.2020040101

Marine Geology & Quaternary Geology > 2020 > 40(4): 40-54. > DOI: 10.16562/j.cnki.0256-1492.2020040101

CHEN Yingying, XIA Fei, ZHANG Zhenke, XU Qinmian, CHEN Shiyue. Research progress on distribution of Quaternary buried paleo-Yangtze River channels in the North Jiangsu-western South Yellow Sea[J]. Marine Geology & Quaternary Geology, 2020, 40(4): 40-54. DOI: 10.16562/j.cnki.0256-1492.2020040101

Citation:

PDF (7406 KB)

Research progress on distribution of Quaternary buried paleo-Yangtze River channels in the North Jiangsu-western South Yellow Sea

1.
School of Geography, Geomatics and Planning, Jiangsu Normal University, Xuzhou 221116, China
2.
School of Urban, Resource and Environmental Sciences, Jiangsu Second Normal University, Nanjing 211200, China
3.
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China
4.
School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210023, China
5.
Tianjin Center of Geological Survey, China Geological Survey, Tianjin 300170, China

More Information

Received Date: March 31, 2020
Revised Date: May 08, 2020
Available Online: August 17, 2020

Graphical Abstract

Abstract

Abstract

Based on published literatures, a thorough review is made on the distribution of Quaternary buried paleo-Yangtze River channels in the region of North Jiangsu and western South Yellow Sea (NJ-WSYS). The review suggests that Quaternary paleo-river channels are particularly developed in the region left behind by the paleo-Yangtze River. Owing to its wide distribution and complex paleogeomorphology, in addition to lack of high-quality sediment cores, low sampling density and limited dating data, there still remains many disputes on the migration pattern of the Yangtze River paleochannels. One view believes that subject to the neotectonic movement, the Quaternary Yangtze River channel flowed into the sea following the variable paths to the south of a line that through Yangzhou, Taizhou, Jiangyan, Haian and Jianggang, however, there are many controversies on the exact location of the estuary for a specific river course. Another view, however, suggests that due to the effect of differential tectonic subsidence and topographic barrier, the paleo-Yangtze River, shifting from the North Jiangsu Plain, flowed towards south and through the northern flank of Yangtze River delta. In addition, a series of nearly EW-trending Yangtze River paleochannels have also been found on the adjacent continental shelf of the western South Yellow Sea, which were formed at the end of Late Pleistocene. As a key research area for the paleo-Yangtze River channel migration, therefore, it is still needed to increase the research resolution of sediment cores, to improve the dating accuracy and resolution of the ages to establish reliable chronostratigraphic frameworks, and to reinforce the analysis of sediment provenance in long time scale and correlation of land-sea sedimentary record in the NJ-WSYS. To ascertain the distribution of buried Yangtze River paleochannels in this area will contribute to the further understanding of the evolution processes and mechanisms of the Quaternary Yangtze River sediment source-to-sink system, enrich the knowledge on the evolution of paleogeomorphology and sedimentary environments, and provide the scientific basis for rational exploitation and utilization of resources and engineering constructions.
- buried paleo-Yangtze River channels,
- sedimentary environment,
- Quaternary,
- North Jiangsu-western South Yellow Sea

FullText(HTML)

References (61)

References

[1]	吴忱. 华北平原古河道研究[M]. 北京: 中国科学技术出版社, 1991. WU Chen. Study on Paleo-Channels of the North China Plain[M]. Beijing: China Science and Technology Press, 1991.
[2]	赵艳霞, 徐全洪, 刘芳圆, 等. 近20年来中国古河道研究进展[J]. 地理科学进展, 2013, 32(1):3-19. [ZHAO Yanxia, XU Quanhong, LIU Fangyuan, et al. Progresses of palaeochannel studies in China in the past 20 years [J]. Progress in Geography, 2013, 32(1): 3-19. doi: 10.11820/dlkxjz.2013.01.001
[3]	鲍才旺. 珠江口陆架区埋藏古河道与古三角洲[J]. 海洋地质与第四纪地质, 1995, 15(2):25-34. [BAO Caiwang. Buried ancient channels and deltas in the Zhujiang River mouth shelf area [J]. Marine Geology & Quaternary Geology, 1995, 15(2): 25-34.
[4]	夏东兴, 刘振夏. 末次冰期盛期长江入海流路探讨[J]. 海洋学报, 2001, 23(5):87-94. [XIA Dongxing, LIU Zhenxia. Tracing the Changjiang River’s flowing route entering the sea during the last ice age maximum [J]. Acta Oceanologica Sinica, 2001, 23(5): 87-94.
[5]	李广雪, 刘勇, 杨子赓, 等. 末次冰期东海陆架平原上的长江古河道[J]. 中国科学D辑: 地球科学, 2004, 35(3):284-289. [LI Guangxue, LIU Yong, YANG Zigeng, et al. Ancient Changjiang channel system in the East China Sea continental shelf during the last glaciation [J]. Science in China Series D: Earth Sciences, 2004, 35(3): 284-289. doi: 10.1360/04yd0053
[6]	Liu J, Saito Y, Kong X H, et al. Delta development and channel incision during marine isotope stages 3 and 2 in the western South Yellow Sea [J]. Marine Geology, 2010, 278(1-4): 54-76. doi: 10.1016/j.margeo.2010.09.003
[7]	孔祥淮, 刘健, 张勇, 等. 南黄海西部滨浅海区埋藏古河道研究[J]. 海洋科学进展, 2013, 31(3):367-376. [KONG Xianghuai, LIU Jian, ZHANG Yong, et al. Study on buried channel systems in the western South Yellow Sea [J]. Advances in Marine Science, 2013, 31(3): 367-376. doi: 10.3969/j.issn.1671-6647.2013.03.009
[8]	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. [SHU Qiang, ZHANG Maoheng, ZHAO Zhijun, 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. doi: 10.3969/j.issn.0253-4959.2008.03.013
[9]	范代读, 李从先, Yokoyama K, et al. 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: 地球科学, 2004, 34(11):1015-1022. [FAN Daidu, LI Congxian, Yokoyama K, et al. Monazite age spectra in the Late Cenozoic of the Changjiang Delta and its implication on the Changjiang run-through time [J]. Science in China (Series D), 2004, 34(11): 1015-1022.
[10]	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(2):299-307. [HUANG Xiangtong, ZHENG Hongbo, YANG Shouye, et al. Investigation of sedimentary geochemistry of Core DY03 in the Yangtze Delta: implications to tracing provenance [J]. Quaternary Sciences, 2009, 29(2): 299-307. doi: 10.3969/j.issn.1001-7410.2009.02.14
[11]	程瑜, 李向前, 赵增玉, 等. 长江三角洲地区TZK3孔碎屑锆石U-Pb年龄及其物源意义[J]. 地质力学学报, 2018, 24(5):635-644. [CHENG Yu, LI Xiangqian, ZHAO Zengyu, et al. Detrital zircon U-Pb ages and its provenance significance in the TZK3 Core from the Yangtze River delta [J]. Journal of Geomechanics, 2018, 24(5): 635-644. doi: 10.12090/j.issn.1006-6616.2018.24.05.064
[12]	孔祥兴, 崔德庚. 江苏省平原区晚新生代以来的古河道[J]. 江苏地质, 1986(2):61-64. [KONG Xiangxing, CUI Degeng. Paleo-channels on plain regions of Jiangsu Province since Late Cenozoic [J]. Jiangsu Geology, 1986(2): 61-64.
[13]	沈国俊. 长江古河道的发现[C]//中国地质学会第四纪冰川与第四纪地质专业委员会. 第四纪冰川与第四纪地质论文集. 北京: 地质出版社, 1988: 203-206. SHEN Guojun. Discovery of paleo-channels of the Yangtze River[C]//Commission on Quaternary Glaciology and Geology of the Geological Society of China. Contribution to the Quaternary Glaciology and Quaternary Geology. Beijing: Geological Publishing House, 1988: 203-206.
[14]	Chen Z Y, Stanley D J. Quaternary subsidence and river channel migration in the Yangtze delta plain, eastern China [J]. Journal of Coastal Research, 1995, 11(3): 927-945.
[15]	李从先, 万明浩, 陈庆强. 苏北沿南-三仓地区的古河谷及其地质意义[J]. 科学通报, 1996, 41(23):2168-2170. [LI Congxian, WAN Minghao, CHEN Qingqiang. Paleovalley in the Yannan-Sancang area of Jiangsu Province and its geological significance [J]. Chinese Science Bulletin, 1996, 41(23): 2168-2170. doi: 10.1007/BF02882549
[16]	仲德林, 申宪忠, 夏东兴, 等. 全新世早期古长江海侵三角洲卫片初步解释[J]. 海洋科学, 1983(2):16-17. [ZHONG Delin, SHEN Xianzhong, XIA Dongxing, et al. Explanation of satellitic photography of the ancient Changjiang Delta region in early Holocene [J]. Marine Sciences, 1983(2): 16-17.
[17]	杨子赓. 南黄海陆架晚更新世以来的沉积及环境[J]. 海洋地质与第四纪地质, 1985, 5(4):1-19. [YANG Zigeng. Sedimentology and environment in South Yellow Sea shelf since late Pleistocene [J]. Marine Geology & Quaternary Geology, 1985, 5(4): 1-19.
[18]	刘奎, 庄振业, 刘冬雁, 等. 长江口外陆架区埋藏古河道研究[J]. 海洋学报, 2009, 31(5):80-88. [LIU Kui, ZHUANG Zhenye, LIU Dongyan, et al. Study of the buried ancient channels in the continental shelf area out of the mouth of the Changjiang River in China [J]. Acta Oceanologica Sinica, 2009, 31(5): 80-88.
[19]	雷宝华, 陈建文, 梁杰, 等. 印支运动以来南黄海盆地的构造变形与演化[J]. 海洋地质与第四纪地质, 2018, 38(3):45-54. [LEI Baohua, CHEN Jianwen, LIANG Jie, et al. Tectonic deformation and evolution of the South Yellow Sea basin since Indosinian movement [J]. Marine Geology & Quaternary Geology, 2018, 38(3): 45-54.
[20]	郑光膺. 黄海第四纪地质[M]. 北京: 科学出版社, 1991. ZHENG Guangying. Quaternary Geology of the South Yellow Sea[M]. Beijing: Science Press, 1991.
[21]	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. [WANG Ying, ZHANG Zhenke, ZHU Dakui, et al. River-sea interaction and the north Jiangsu Plain formation [J]. Quaternary Sciences, 2006, 26(3): 301-320. doi: 10.3321/j.issn:1001-7410.2006.03.001
[22]	Liu J, Zhang X H, Mei X, et al. The sedimentary succession of the last~3.50 Myr in the western South Yellow Sea: Paleoenvironmental and tectonic implications [J]. Marine Geology, 2018, 399: 47-65. doi: 10.1016/j.margeo.2017.11.005
[23]	中国地图出版社. 江苏省地图集[M]. 北京: 中国地图出版社, 2004. China Map Press. Atlas of the Jiangsu Province[M]. Beijing: China Cartographic Publishing House, 2004.
[24]	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. LI Congxian, WANG Pinxian. Late Quaternary Stratigraphy of the Changjiang Delta[M]. Beijing: Science Press, 1998.
[25]	陈影影. 中更新世以来长江三角洲北翼沉积环境与物源演变[D].南京大学博士学位论文, 2016. CHEN Yingying. Evolution of depositional environment and sediment sources of the northern Yangtze River Delta since the middle Pleistocene[D]. Doctor Dissertation of Nangjing University, 2016.
[26]	季云. 苏北海岸带弶港钻孔沉积相及沉积环境演化[D]. 南京大学硕士学位论文, 2015. JI Yun. The core-recorded and sedimentary facies of late Pleistocene-Holocene environment evolution, Jianggang, northern Jiangsu coast, South Yellow Sea, eastern China[D]. Master Dissertation of Nangjing University, 2015.
[27]	郑光膺. 南黄海第四纪层型地层对比[M]. 北京: 科学出版社, 1989. ZHENG Guangying. The Stratigraphic Correlation of the Quaternary Stratotype in the South Yellow Sea[M]. Beijing: Science Press, 1989.
[28]	Li C X, Wang P, Sun H P, et al. Late Quaternary incised-valley fill of the Yangtze delta (China): its stratigraphic framework and evolution [J]. Sedimentary Geology, 2002, 152(1-2): 133-158. doi: 10.1016/S0037-0738(02)00066-0
[29]	江苏省地质矿产局第二水文地质工程地质大队. 江苏省徐淮盐地区水文地质工程地质综合评价报告(1: 50万)[R]. 1985. The Second Hydrological Engineering Team of Jiangsu Geology and Mine Bureau. Comprehensive evaluation report of hydrogeology and engineering geology of Xuzhou-Huaian-Yancheng, Jiangsu Province (1/500000)[R]. 1985.
[30]	顾家伟. 上新世以来苏北盆地与长江三角洲构造沉降史分析[J]. 地质科技情报, 2015, 34(1):95-99, 106. [GU Jiawei. Tectonic subsidence analysis of Subei Basin and Yangtze Delta from the pliocene [J]. Geological Science and Technology Information, 2015, 34(1): 95-99, 106.
[31]	吴标云, 李从先. 长江三角洲第四纪地质[M]. 北京: 海洋出版社, 1987. WU Biaoyun, LI Congxian. Quaternary Geology of the Yangtze River Delta[M]. Beijing: China Ocean Press, 1987.
[32]	江苏省地质调查研究院. 长江三角洲地区(长江以北)环境地质综合调查评价报告[R]. 2012. Geological Survey of Jiangsu Province. Comprehensive investigation and evaluation report of environmental geology of the Yangtze River Delta (northern Yangze River)[R]. 2012.
[33]	江苏地质局第一水文地质队. 镇江幅、高邮幅1: 20万区域水文地质普查报告[R]. 1980. The First Hydrological Engineering Team of Jiangsu Geology Bureau. 1/200000 regional hydrogeological survey report of Zhenjiang and Gaoyou[R]. 1980.
[34]	耿秀山. 中国东部陆架的海底古河系[J]. 海洋科学, 1981(2):21-26. [GENG Xiushan. Submarine paleochannel systems on the continental shelf of eastern China [J]. Marine Sciences, 1981(2): 21-26.
[35]	杨子赓. 晚松山时南黄海的古长江三角洲[J]. 第四纪研究, 1994(1):13-23. [YANG Zigeng. Palaeo-Yangtze River Delta in the South Yellow Sea during late Matuyama chron [J]. Quaternary Sciences, 1994(1): 13-23. doi: 10.3321/j.issn:1001-7410.1994.01.002
[36]	顾兆峰, 张志珣. 南黄海西部浅部地层地震层序及其沉积特征[J]. 海洋地质与第四纪地质, 2009, 29(4):95-106. [GU Zhaofeng, ZHANG Zhixun. Shallow seismic stratigraphy and sedimentary character in the western South Yellow Sea [J]. Marine Geology & Quaternary Geology, 2009, 29(4): 95-106.
[37]	阚为群. 苏北中部沿海平原全新世沉积环境演变[D]. 华东师范大学, 1988. KAn Weiqun. Evolution of the Holocene sedimentary environment of the coast plain in the middle-north of Jiangsu Province[D]. East China Normal University, 1988.
[38]	李从先, 张桂甲. 末次冰期时存在入海的长江吗?[J]. 地理学报, 1995, 50(5):459-463. [LI Congxian, ZHANG Guijia. A sea-running Changjiang River during the last glaciation? [J]. Acta Geographica Sinica, 1995, 50(5): 459-463. doi: 10.3321/j.issn:0375-5444.1995.05.009
[39]	秦蕴珊, 李凡, 唐宝珏, 等. 南黄海西部埋藏古河系[J]. 科学通报, 1986(24):1887-1890. [QIN Yunshan, LI Fan, TANG Baojue, et al. Buried paleo-channels in the South Yellow Sea [J]. Chinese Science Bulletin, 1986(24): 1887-1890.
[40]	王颖, 朱大奎, 周旅复, 等. 南黄海辐射沙脊群沉积特点及其演变[J]. 中国科学(D辑), 1998, 28(5):385-393. [WANG Ying, ZHU Dakui, ZHOU Lvfu, et al. Evolution of radiative sand ridge field of the South Yellow Sea and its sedimentary characteristics [J]. Science in China Series D: Earth Sciences, 1998, 28(5): 385-393. doi: 10.1007/BF02878503
[41]	李凡, 于建军, 姜秀珩, 等. 南黄海埋藏古河系研究[J]. 海洋与湖沼, 1991, 22(6):501-508. [LI Fan, YU Jianjun, JIANG Xiuhang, et al. Study on buried paleo-channel system in the South Yellow sea [J]. Oceanologia et Limnologia Sinica, 1991, 22(6): 501-508.
[42]	李晶, 张志, 张维冈, 等. 南黄海浅部埋藏古地貌的特征、分布及其工程影响[J]. 海洋地质前沿, 2011, 27(8):48-52. [LI Jing, ZHANG Zhi, ZHANG Weigang, et al. Shallowly-buried paleo-geomorphological features and distribution in the South Yellow Sea and their influence on marine engineering [J]. Marine Geology Frontiers, 2011, 27(8): 48-52.
[43]	刘敏厚, 吴世迎, 王永吉. 黄海晚第四纪沉积[M]. 北京: 海洋出版社, 1987. LIU Minhou, WU Shiying, WANG Yongji. Sedimentology of the Yellow Sea During the Late Quaternary[M]. Beijing: China Ocean Press, 1987.
[44]	王辉, 夏非, 张永战, 等. 江苏中部海岸西洋潮流通道区域晚更新世古地貌与沉积体系研究[J]. 海洋学报, 2019, 41(3):134-142. [WANG Hui, XIA Fei, ZHANG Yongzhan, et al. Paleo-geomorphology and sedimentary systems of the Xiyang tidal channel on the central Jiangsu coast at the late Pleistocene [J]. Haiyang Xuebao, 2019, 41(3): 134-142.
[45]	孙顺才. 长江三角洲全新世沉积特征[J]. 海洋学报, 1981, 3(1):97-113. [SUN Shuncai. Deltaic sediments of the Changjing delta and its characteristics [J]. Acta Oceanologica Sinica, 1981, 3(1): 97-113.
[46]	杨怀仁, 韩同春, 杨达源, 等. 长江下游晚更新世以来河道变迁的类型与机制[J]. 南京大学学报: 自然科学版, 1983(2):341-350. [YANG Huairen, HAN Tongchun, YANG Dayuan, et al. Processes and causal mechanism of migrations of the Changjiang (Yangtze river) since late pleistocene [J]. Journal of Nanjing University: Natural Sciences, 1983(2): 341-350.
[47]	曹光杰, 王建, 屈贵贤. 末次盛冰期以来长江河口段河道演变研究综述[J]. 地球科学进展, 2006, 21(10):1039-1045. [CAO Guangjie, WANG Jian, QU Guixian. An overview of the research on channel evolution in the Yangtze River mouth region since the Last Glacial Maximum [J]. Advances in Earth Science, 2006, 21(10): 1039-1045. doi: 10.3321/j.issn:1001-8166.2006.10.007
[48]	李庆忠. 近代河流沉积与地震地层学解释[J]. 石油物探, 1994, 33(2):26-41. [LI Qingzhong. Recent river sediments and seismic stratigraphic interpretation [J]. Geophysical Prospecting for Petroleum, 1994, 33(2): 26-41.
[49]	王富葆, 曹琼英, 李弘, 等. 上海市15-17 kaBP的古地貌与工程地质条件[J]. 上海地质, 2002(83):19-24. [WANG Fubao, CAO Qiongying, LI Hong, et al. Paleogeomorphology and its engineering geological significance during 15-17 kaBP in Shanghai urban area [J]. Shanghai Geology, 2002(83): 19-24.
[50]	高抒. 中国东部陆架全新世沉积体系: 过程—产物关系研究进展评述[J]. 沉积学报, 2013, 31(5):845-855. [GAO Shu. Holocene sedimentary systems over the Bohai, Yellow and East China Sea region: recent progress in the study of process-product relationships [J]. Acta Sedimentologica Sinica, 2013, 31(5): 845-855.
[51]	Liu Z X, Xia D X, Berne S, et al. Tidal deposition systems of China’s continental shelf, with special reference to the eastern Bohai Sea [J]. Marine Geology, 1998, 145(3-4): 225-253. doi: 10.1016/S0025-3227(97)00116-3
[52]	业渝光, 刁少波, 和杰, 等. 南黄海QC<sub>2</sub>孔的ESR年代学[J]. 海洋地质与第四纪地质, 1996, 16(1):95-102. [YE Yuguang, DIAO Shaobo, HE Jie, et al. ESR chronology of well QC<sub>2</sub> in the South Yellow Sea [J]. Marine Geology & Quaternary Geology, 1996, 16(1): 95-102.
[53]	夏非, 张永战. 苏北平原龙冈LG孔晚第四纪地层与环境演化记录[J]. 地理研究, 2018, 37(2):433-446. [XIA Fei, ZHANG Yongzhan. Late Quaternary strata and environmental evolution record of core LG in Longgang, north Jiangsu plain, China [J]. Geographical Research, 2018, 37(2): 433-446.
[54]	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. [ZHANG Zhenke, XIE Li, ZHANG Yunfeng, et al. Sedimentary records of the MIS 3 transgression event in the north Jiangsu plain, China [J]. Quaternary Sciences, 2010, 30(5): 883-891. doi: 10.3969/j.issn.1001-7410.2010.05.05
[55]	谢志仁. 江浙沿海平原及相邻陆架区一万八千年以来的海面变化[D]. 南京大学硕士学位论文, 1981. XIE Zhiren. Sea level changes since 18 ka BP in the coastal plain of Jiangsu and Zhejiang province and its adjacent continental shelf area[D].Master Dissertation of Nanjing University, 1981.
[56]	陈报章, 李从先, 业治铮. 长江三角洲北翼全新统底界和“硬粘土层”的讨论[J]. 海洋地质与第四纪地质, 1991, 11(2):37-46. [CHEN Baozhang, LI Congxian, YE Zhizheng. Holocene bottom boundary and “hardclay band” in the northern flank of the Changjiang River Delta [J]. Marine Geology & Quaternary Geology, 1991, 11(2): 37-46.
[57]	Chen J, Wang Z H, Chen Z Y, et al. Diagnostic heavy minerals in Plio-Pleistocene sediments of the Yangtze Coast, China with special reference to the Yangtze River connection into the sea [J]. Geomorphology, 2009, 113(3-4): 129-136. doi: 10.1016/j.geomorph.2009.03.010
[58]	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. [ZHANG Yufen, LI Changan, WANG Qiuliang, et al. Magnetism parameters characteristics of drilling deposits in Jianghan Plain and indication for forming of the Yangtze River Three Gorges [J]. Chinese Science Bulletin, 2008, 53(5): 577-582. doi: 10.1007/s11434-008-0111-1
[59]	王节涛, 李长安, 杨勇, 等. 江汉平原周老孔中碎屑锆石LA-ICPMS定年及物源示踪[J]. 第四纪研究, 2009, 29(2):343-351. [WANG Jietao, LI Changan, YANG Yong, et al. The LA-ICPMS U-Pb detrital zircon geochronology and provenance study of sedimentary core in the Zhoulao town, the Jianghan Plain, China [J]. Quaternary Sciences, 2009, 29(2): 343-351. doi: 10.3969/j.issn.1001-7410.2009.02.19
[60]	Zhang J, Wan S M, Clift P D, et al. History of Yellow River and Yangtze River delivering sediment to the Yellow Sea since 3.5 Ma: Tectonic or climate forcing? [J]. Quaternary Science Reviews, 2019, 216: 74-88. doi: 10.1016/j.quascirev.2019.06.002
[61]	陈静, 王哲, 王张华, 等. 长江三角洲东西部晚新生代地层中的重矿物差异及其物源意义[J]. 第四纪研究, 2007, 27(5):700-708. [CHEN Jing, WANG Zhe, WANG Zhanghua, 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. doi: 10.3321/j.issn:1001-7410.2007.05.011