SEISMOLOGY AND GEOLOGY ›› 2004, Vol. 26 ›› Issue (1): 24-32.

• Brief Report • Previous Articles     Next Articles

DEVELOPMENT OF THE QUATERNARY SYSTEM IN THE BOHAI SEA AREA, CHINA

XU Jie, RAN Yong-kang, SHAN Xin-jian, CHEN Guo-guang, LI Xiang-gen   

  1. Institute of Geology, China Earthquake Administration, Beijing 100029, China
  • Received:2002-10-28 Revised:2003-06-29 Online:2004-03-04 Published:2009-10-26

渤海海域第四系发育概况

徐杰, 冉勇康, 单新建, 陈国光, 李祥根   

  1. 中国地震局地质研究所, 北京, 100029
  • 作者简介:徐杰,男,1967年毕业于南京大学地质系大地构造专业,1986年在中国科学技术大学研究生院和国家地震局地质研究所获博士学位,研究员,博士生导师,主要从事地震构造、新构造和盆地构造等研究,电话:010-62009154.
  • 基金资助:
    国家重点基础研究发展规划项目(G1998040701)和中国地质调查局基础地质综合研究项目(200113000053)共同资助.

Abstract: The Bohai Sea is located in the east of the Bohai Bay Cenozoic rift basin, and has been characterized by intense tectonic activities since Quaternary time. Many major earthquakes of M≥7 had occurred in this area in history. Although a great number of detailed studies on the land part of the basin have been made, little has been done on the research of the Quaternary sediments in the Bohai Sea area. The isopach map of Quaternary system for this area has not been compiled so far. Basing on the previous studies, we used the data of the thickness of Neogene - Quaternary system, and the thickness of the Guantao and Minghuazhen Groups of Neogene to compile the isopach map of the Quaternary system with the help of GIS and image processing. This map shows that the Quaternary system is generally 300~600m thick, and locally 800~1000m thick in the studied area. The isopach in the western and eastern parts of the Bohai Sea exhibits NW- and NE-trending belt-like shape, respectively.

Key words: isopach map of Quaternary system, Bohai Bay basin, Bohai Sea

摘要: 渤海位于渤海湾新生代裂陷盆地的东部.该区第四纪构造活动强烈,历史上发生过多次7级以上地震.然而,渤海地区第四系的研究远不能与渤海湾盆地的陆地部分相比,有关第四系厚度分布的情况至今仍未见报道.为此,文中在综合已有研究成果的基础上,还利用新近系-第四系、新近系馆陶组和明化镇组的厚度分布资料,通过GIS与图像处理相结合的方法,编制了第四系厚度分布图.渤海地区第四系一般厚300~600m,局部厚达800~1 000m;渤海西部和东部第四系等厚线总体分别呈NW和NE向带状分布.

关键词: 第四系厚度分布, 渤海湾盆地, 渤海

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