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渤海湾晚更新世晚期以来古河道分布和三角洲发育及其古环境的演变

雷雁翔, 何磊, 叶思源, 赵俐红, 袁红明, 杨士雄, 薜春汀, EdwardA. Laws. 2021. 渤海湾晚更新世晚期以来古河道分布和三角洲发育及其古环境的演变[J]. 中国地质, 48(6): 1947-1964. doi: 10.12029/gc20210621
引用本文: 雷雁翔, 何磊, 叶思源, 赵俐红, 袁红明, 杨士雄, 薜春汀, EdwardA. Laws. 2021. 渤海湾晚更新世晚期以来古河道分布和三角洲发育及其古环境的演变[J]. 中国地质, 48(6): 1947-1964. doi: 10.12029/gc20210621
LEI Yanxiang, HE Lei, YE Siyuan, ZHAO Lihong, YUAN Hongming, YANG Shixiong, XUE Chunting, Edward A. Laws. 2021. Paleochannel distribution, delta development and paleoenvironment evolution in Bohai Bay since the Late Pleistocene[J]. Geology in China, 48(6): 1947-1964. doi: 10.12029/gc20210621
Citation: LEI Yanxiang, HE Lei, YE Siyuan, ZHAO Lihong, YUAN Hongming, YANG Shixiong, XUE Chunting, Edward A. Laws. 2021. Paleochannel distribution, delta development and paleoenvironment evolution in Bohai Bay since the Late Pleistocene[J]. Geology in China, 48(6): 1947-1964. doi: 10.12029/gc20210621

渤海湾晚更新世晚期以来古河道分布和三角洲发育及其古环境的演变

  • 基金项目:
    科技部政府间科技创新合作重点专项(2016YFE0109600),中国地质调查局项目(DD20160144,DD20189503)和国家自然科学基金(41706057,41876057)联合资助
详细信息
    作者简介: 雷雁翔, 男, 1994年生, 硕士, 地球化学专业; E-mail: 479536119@qq.com
    通讯作者: 叶思源, 女, 1963年生, 研究员, 主要从事海洋地质、地球化学研究; E-mail: siyuanye@hotmail.com
  • 中图分类号: P736.2

Paleochannel distribution, delta development and paleoenvironment evolution in Bohai Bay since the Late Pleistocene

  • Fund Project: Supported by the key project of Intergovernmental Scientific and Technological Innovation Cooperation of the Ministry of Science and Technology (No.2016yfe0109600), the project of China Geological Survey (No.DD20160144, No. DD20189503) and the National Natural Science Foundation of China (No.41706057, No.41876057)
More Information
    Author Bio: LEI Yanxiang, male, born in 1994, master, engaged in the study of geochemistry; E-mail: 479536119@qq.com .
    Corresponding author: YE Siyuan, female, born in 1963, senior researcher, engaged in the study of marine geology and geochemistry; E-mail: siyuanye@hotmail.com
  • 渤海湾及其沿岸是中国海洋地质与第四纪地质研究程度最高的地区之一。虽然研究成果众多,但仍有一些基础的地质问题亟待解决。比如,晚更新世晚期黄河是否流经渤海湾?全新世黄河在渤海湾及其沿岸形成的多期次三角洲叶瓣在海域如何展布?以上问题一直是中国海洋地质研究中备受关注的热点话题。借助2016-2017年在渤海湾获取的约2000 km的浅地层剖面数据、2个30 m左右的取芯钻孔(BXZK2017-1和BXZK2017-2孔)及相应的AMS 14C和OSL测年数据,同时结合前人的一些浅剖数据和钻孔的研究成果,将渤海湾中部晚更新世以来的地层自上而下划分出4个地震单元(SU1~SU4)和6个沉积单元(DU1-DU6),分别对应前三角洲相、潮坪与浅海、泛滥平原、河道相、海陆交互相、湖沼相。在此基础上综合探讨渤海湾晚更新世晚期以来总体的地层框架和沉积演化特征。研究表明:黄河可能在21.8~9 cal ka BP,由近东西向流经渤海湾北部进入渤海中部盆地;全新世以来,渤海湾从西北侧至南侧,依次分布4期次的三角洲叶瓣,对应的发育时间可能分别是1400 AD~现在、11~1128 AD、700 BC~11 AD和1855~现在;渤海湾西侧最北两期次的水下三角洲可能主要与海河有关,而南侧其余2期次三角洲叶瓣则可能分别对应岐口超级叶瓣以及现代黄河三角洲超级叶瓣。加深了解渤海湾晚更新世晚期以来的地层序列演化、古河道发育以及全新世三角洲在渤海湾的展布情况,将有助于渤海湾海岸带开发、海底工程建设以及地质灾害防范等。

  • 加载中
  • 图 1  渤海湾浅地层剖面测线和钻孔位置分布图

    Figure 1. 

    图 2  钻孔BHZK2017-1、BHZK2017-2地层对比图

    Figure 2. 

    图 3  渤海湾钻孔中典型的沉积相及沉积特征

    Figure 3. 

    图 4  测线L2、Z7浅剖剖面图

    Figure 4. 

    图 5  地震单元层等深图(a、b、c、d分别是H0、H1、H2、H4层)

    Figure 5. 

    图 6  地震单元层等厚图(a、b、c分别是是SU1、SU2、SU3)

    Figure 6. 

    图 7  渤海湾钻孔晚更新世以来的区域地层对比

    Figure 7. 

    图 8  渤海湾古河道及水下三角洲范围分布图

    Figure 8. 

    图 9  典型古河道和三角洲叶瓣浅剖分析图

    Figure 9. 

    表 1  渤海湾地区钻孔位置

    Table 1.  Location of boreholes in Bohai Bay

    下载: 导出CSV

    表 2  渤海湾钻孔AMS 14C测年数据

    Table 2.  List of AMS 14C ages from boreholes in Bohai Bay

    下载: 导出CSV

    表 3  渤海湾钻孔光释光(OSL)测年数据

    Table 3.  List of OSL ages from boreholes in Bohai Bay

    下载: 导出CSV
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出版历程
收稿日期:  2019-05-11
修回日期:  2019-11-18
刊出日期:  2021-12-25

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