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河海交互作用与苏北平原成因
  • ISSN号:1001-7410
  • 期刊名称:《第四纪研究》
  • 时间:0
  • 分类:P736[天文地球—海洋地质;天文地球—海洋科学] P737[天文地球—海洋地质;天文地球—海洋科学]
  • 作者机构:[1]南京大学海岸与海岛开发教育部重点实验室,南京 210093, [2]南京大学海洋地球化学研究中心,南京 210093
  • 相关基金:国家自然科学基金项目(批准号:40271004)资助
中文摘要:

苏北平原向海侧分布着大冈、上冈两列古贝壳堤以及依此而建的范公堤;西侧有低山丘陵环绕,江淮水系河流汇入平原内侧的湖泊群,发育了伸出型三角洲;兴化、里下河地区是平原的最低洼处.这一系列地貌组合与分布特点,启迪着探究平原的成因.146m深的宝应望直港钻孔,穿透了2.58Ma以来的第四纪地层.沉积相、微体古生物、古地磁测定与沉积层常量元素分析等综合研究,阐明了4次主要的海洋作用沉积环境,尤其是晚更新世3.9~2.6万年前的浅海环境沉积更为显著.河湖相泛滥平原沉积与潮滩浅海沉积交互成层,证实了苏北平原是第四纪时期由河-海交互作用,从古海湾发育堆积成宽大平原.进一步工作需探索相关时期的江-海分布变化及黄河和黄渤海通道与苏北平原发育的关系.

英文摘要:

The North Jiangsu Plain is located on the northern side of the Changjiang River and the south of Lan-Shan-Tou Cape in the area of 32°10′ -35°05′N and 118°40′ -120°30′E. The landform is mainly lowland declined from the Grand Canal in the west towards the east along the Yellow Sea coast, with the lowest place around the Xinhua-Sheyang lake area in the middle of the plain. A sufficient water network of rivers, canals and lakes is the major feature of the plain with the abandoned Huanghe River-Huaihe River system in the north, and the Changjiang River system and numerous lakes in the south. Previous studies have discovered that the eastern part of the plain was formed from the sea during Holocene high sea level period which is evidenced by a series of shell beach ridges located in Longgang, Dagang, Dongtai, and Hai'an for about 200km long from north to south, about 60km west of the present coastline. ^14C datings have shown that it was formed 6500 ~ 5600aB. P. A manmade dike, named Fan-Gong Dike, was built combined with the shell beach ridges to form a complete dike during 960 ~ 1127A. D. This study is to trace the genetic formation of the plain inside of this old dike. Geomorphologic features of the plain west to the Fan-Gong dike indicate seemingly its following natures : ( 1 ) The North Jiangsu Plain is circumscribed by a series of rocky hills as an arc-shaped "Bay". (2) A series of lakes such as the Hongze Lake, the Gaoyou Lake, and the Shaobo Lake, located on the west side of the Grand Canal, are almost connected to each other either by lowlands or by swamps. There are several rivers entering into these lakes with deltaic forms on the west shore of the lakes. The Grand Canal was actually built by partly using this series of connected lakes. (3) A series of manmade islands were built based on the natural bars or barriers of the lakes or water swamps. These islands are locally named as Duo, Dun or Wei, each of which in Chinese means "manmade bar or crossway". These islan

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期刊信息
  • 《第四纪研究》
  • 中国科技核心期刊
  • 主管单位:中国科学院
  • 主办单位:中国科学院地质与地球物理研究所 中国第四纪研究委员会
  • 主编:郭正堂
  • 地址:北京9825信箱
  • 邮编:100029
  • 邮箱:dsj@mail.igcas.ac.cn dsjs@mail.igcas.ac.cn
  • 电话:010-82998119
  • 国际标准刊号:ISSN:1001-7410
  • 国内统一刊号:ISSN:11-2708/P
  • 邮发代号:82-428
  • 获奖情况:
  • 1996年被国务院学位委员会地球物理及地质学科评议...,2001年入中国期刊方阵,2007年获中国科学院出版基金科技期刊排行榜三等奖
  • 国内外数据库收录:
  • 美国化学文摘(网络版),英国动物学记录,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:17826