南黄海盆地南部海相构造层研究新进展

杨艳秋, 李森, 梁杰, 孙晶. 南黄海盆地南部海相构造层研究新进展[J]. 海洋地质前沿, 2025, 41(2): 12-20. doi: 10.16028/j.1009-2722.2024.170
引用本文: 杨艳秋, 李森, 梁杰, 孙晶. 南黄海盆地南部海相构造层研究新进展[J]. 海洋地质前沿, 2025, 41(2): 12-20. doi: 10.16028/j.1009-2722.2024.170
YANG Yanqiu, LI Sen, LIANG Jie, SUN Jing. New progress of research on marine stratum in the southern part of South Yellow Sea Basin[J]. Marine Geology Frontiers, 2025, 41(2): 12-20. doi: 10.16028/j.1009-2722.2024.170
Citation: YANG Yanqiu, LI Sen, LIANG Jie, SUN Jing. New progress of research on marine stratum in the southern part of South Yellow Sea Basin[J]. Marine Geology Frontiers, 2025, 41(2): 12-20. doi: 10.16028/j.1009-2722.2024.170

南黄海盆地南部海相构造层研究新进展

  • 基金项目: 崂山实验室科技创新项目(LSKJ202203401,LSKJ202203404);中国地质调查局项目(DD20190818,DD20221723,DD20230317,DD2024-1723,DD20243116);国家自然科学基金(42076220)
详细信息
    作者简介: 杨艳秋(1976—),女,硕士,正高级工程师,主要从事海洋油气地质方面的研究工作. E-mail:qimgyyq@126.com
    通讯作者: 梁杰(1979—),男,博士,正高级工程师,主要从事海域油气资源调查方面的研究工作. E-mail:lj_100@163.com
  • 中图分类号: P744.4;P736

New progress of research on marine stratum in the southern part of South Yellow Sea Basin

More Information
  • 以南黄海盆地南部为研究区,二叠系上统—三叠系下统为研究对象,根据近年来新采集和处理的二维地震资料,对该区域的海相构造层进行了深入分析,取得了一些新的地质认识。研究表明:南黄海盆地南部广泛发育早三叠世—晚二叠世地层,最大残留厚度超过3 000 m;海相构造层的断裂系统主要呈NW—NWW和近EW走向,发育海相中—古生界的挤压断裂体系和陆相中—新生界的拉张断裂体系;根据断裂发育时间,可将其活动期次划分为印支期和燕山-喜山期;同时,根据断裂的平面展布及组合特征,可划分出4类构造样式和9种断裂组合。通过对油气地质条件的分析认为,上古生界是南黄海盆地南部海相构造层的油气勘探方向。该研究成果为南黄海海相油气勘探提供了新的拓展区域。

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  • 图 1  南黄海盆地构造单元划分示意图

    Figure 1. 

    图 2  南黄海盆地南部二叠系上统—三叠系下统地震反射特征

    Figure 2. 

    图 3  南黄海盆地南部典型地震剖面

    Figure 3. 

    图 4  南黄海盆地南部三叠系下统厚度图

    Figure 4. 

    图 5  南黄海盆地南部二叠系上统厚度图

    Figure 5. 

    图 6  南黄海盆地南部二叠系上统—三叠系下统断裂系统分布

    Figure 6. 

    图 7  南黄海盆地南部二叠系上统—三叠系下统断裂组合

    Figure 7. 

    表 1  南黄海盆地南部主要构造样式

    Table 1.  Main structural styles in the southern part of the South Yellow Sea Basin

    类型 构造组合 特征剖面
    挤压构
    造样式
    宽缓褶皱
    断展褶皱
    叠瓦状逆冲
    冲起构造
    反转构造样式 正反转构造
    负反转构造
    走滑构
    造样式
    正花状构造
    拉张构造样式 半地堑
    地堑
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收稿日期:  2024-07-16
刊出日期:  2025-02-28

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