中国近海新构造活动断裂调查与地震勘探方法

吴德城, 侯方辉, 祁江豪, 朱晓青. 中国近海新构造活动断裂调查与地震勘探方法[J]. 海洋地质与第四纪地质, 2020, 40(6): 121-132. doi: 10.16562/j.cnki.0256-1492.2020091101
引用本文: 吴德城, 侯方辉, 祁江豪, 朱晓青. 中国近海新构造活动断裂调查与地震勘探方法[J]. 海洋地质与第四纪地质, 2020, 40(6): 121-132. doi: 10.16562/j.cnki.0256-1492.2020091101
WU Decheng, HOU Fanghui, QI Jianghao, ZHU Xiaoqing. Seismic survey and exploration methods for Neotectonic active faults in the area off China continent[J]. Marine Geology & Quaternary Geology, 2020, 40(6): 121-132. doi: 10.16562/j.cnki.0256-1492.2020091101
Citation: WU Decheng, HOU Fanghui, QI Jianghao, ZHU Xiaoqing. Seismic survey and exploration methods for Neotectonic active faults in the area off China continent[J]. Marine Geology & Quaternary Geology, 2020, 40(6): 121-132. doi: 10.16562/j.cnki.0256-1492.2020091101

中国近海新构造活动断裂调查与地震勘探方法

  • 基金项目: 国家自然科学基金 “琉球海沟俯冲带岩石圈结构与流体循环—海洋大地电磁与地震数据约束”(91958210);国家海洋地质专项项目(DD20190365,DD20190377);青岛海洋科学与技术国家实验室鳌山科技创新计划项目“亚洲大陆边缘地质过程与资源环境效应”(2015ASKJ03)
详细信息
    作者简介: 吴德城(1995—),男,硕士研究生,主要从事海洋地质方面的研究,E-mail:wdch1234567@163.com
    通讯作者: 侯方辉(1979—),男,博士,高级工程师,主要从事构造地质和海洋地球物理等研究,E-mail:houfanghui3993@163.com
  • 中图分类号: P714

Seismic survey and exploration methods for Neotectonic active faults in the area off China continent

More Information
  • 中国近海处于大洋板块与大陆板块作用的关键区域,新构造运动频繁,活动断裂是其主要的表现形式之一。浅地层剖面仪测量、单道地震、多道地震和海底地震仪探测(OBS)等海洋地震勘探方法是调查研究海域活动断裂的主要地球物理手段,各自具有不同技术优势和探测功能,在海域活动断裂调查研究中发挥了重要作用。通过OBS广角反射/折射深地震探测和长排列多道地震勘探,获得了中国近海的区域深大断裂展布特征,深化了深大断裂形成与演化的深部动力学机理的认识,进而分析了其对活动断裂控制与约束关系。根据活动断裂时代新、埋藏浅的特点,综合利用浅地层剖面仪测量、单道地震和高分辨率多道地震方法,获得了中国近海海域活动断裂的分布、走向和差异升降等特征,分析了新构造运动的演化规律。本文综述了海洋地震勘探技术方法的主要特点和功能,及其在海域活动断裂调查中的功能和作用,总结了利用地震勘探技术方法在中国近海新构造活动断裂调查研究中取得的主要成果,提出了在未来的海域新构造运动地震调查研究中,应采用多技术方法组合系统调查与研究的思路,着力提高地震勘探的精度,探索应用横波地震勘探和海底可控震源等新技术的建议。

  • 加载中
  • 图 1  中国近海区域性深大断裂和活动断裂分布示意图[2-3]

    Figure 1. 

    图 2  南黄海典型的浅部地层声学剖面

    Figure 2. 

    图 3  过CSDP-2井典型的高分辨率多道地震剖面

    Figure 3. 

    图 4  南黄海OBS-2013线纵波速度结构剖面[44]

    Figure 4. 

    图 5  渤海海峡调查区断裂分布示意图

    Figure 5. 

    图 6  多道地震呈现的千里岩断裂活动特征

    Figure 6. 

    图 7  东海陆架盆地多道地震显示继承深大断裂的活动断层

    Figure 7. 

    表 1  主要地震勘探方法对比

    Table 1.  Comparison of main seismic exploration methods

    探测方法分辨率勘探深度工作方式主要用途
    浅地层剖面20~50 cm100 m左右电火花震源激发,拖曳式单道接收用于全新世地质特征和活动断裂探查
    单道地震2~5 m(和震源的激发能量有关)500~1000 m(和震源的激发能量有关)电火花震源或小容量气枪激发,拖曳式单道接收用于第四纪地质特征和活动断裂探查与成岩基底相关的活动断裂探查
    高分辨率多道地震1~3 m1000~1500 m大能量电火花或相干气枪激发,小间距多道接收用于新生代地质特征和活动断裂探查与成岩基底相关的活动断裂探查
    长排列多道地震几十米到几百米几千米到上万米大能量气枪阵列震源激发,长排列多道接收,道数可达几百道用于区域地质和探查盆地基底
    海底地震仪(OBS)分辨率低,只反映地层宏观速度结构可达莫霍面大能量气枪枪阵激发,单点独立式接收用于探查地壳构造、深部断裂和中到深大断裂
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出版历程
收稿日期:  2020-09-11
修回日期:  2020-10-02
刊出日期:  2020-12-25

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