南海主要断裂(带)与构造分区

邱燕, 杜文波, 鞠东, 韩冰, 马浩明, 胡小三. 南海主要断裂(带)与构造分区[J]. 海洋地质与第四纪地质. doi: 10.16562/j.cnki.0256-1492.2023070701
引用本文: 邱燕, 杜文波, 鞠东, 韩冰, 马浩明, 胡小三. 南海主要断裂(带)与构造分区[J]. 海洋地质与第四纪地质. doi: 10.16562/j.cnki.0256-1492.2023070701
QIU Yan, DU Wenbo, JU Dong, HAN Bing, MA Haoming, HU Xiaosan. Main faults and tectonic divisions in the South China Sea[J]. Marine Geology & Quaternary Geology. doi: 10.16562/j.cnki.0256-1492.2023070701
Citation: QIU Yan, DU Wenbo, JU Dong, HAN Bing, MA Haoming, HU Xiaosan. Main faults and tectonic divisions in the South China Sea[J]. Marine Geology & Quaternary Geology. doi: 10.16562/j.cnki.0256-1492.2023070701

南海主要断裂(带)与构造分区

  • 基金项目: 广东省特支计划(GML2019BT02H594);中国地质调查局项目(DD20221712,DD20240090)
详细信息
    作者简介: 邱燕 (1956—),女,博士,正高级工程师,从事石油地质、大地构造与海洋地质研究,E-mail:zqiuyan60@163. com
  • 中图分类号: P736.1

Main faults and tectonic divisions in the South China Sea

  • 构造分区是区域构造演化研究的基础。由于区域性构造分区的界线基本上都以深大断裂(带)为依据,因此在划分构造单元之前,研究区域内规模较大的主要断裂(带)是必不可少的。本文在分析南海主要断裂(带)的基础上,以板块构造理论为指导,完善了南海的构造分区。南海主要断裂(带)分为以俯冲带、碰撞带、大型逆冲带、大型走滑带为特征的一级断裂带;切穿沉积基底与上地壳、延伸至下地壳的二级断裂带;错断沉积基底的三级断裂。本区一级构造单元为“南海次板块”,其边界基本以一级断裂带,个别以二级断裂带为界;二级构造单元有微板块、断阶带、隆起区、深坳带、深坳区、碰撞带等;三级构造单元在微板块之内划分为隆坳带和微地块。

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  • 图 1  南海地形地貌与测线位置图

    Figure 1. 

    图 2  南海主要断裂(带)分布图[10]

    Figure 2. 

    图 3  St地震剖面示南海北部陆架至陆坡三级断裂特征

    Figure 3. 

    图 4  西沙海槽断裂带构造特征

    Figure 4. 

    图 5  莺歌海盆地内的莺东断裂

    Figure 5. 

    图 6  位于南海西部陆缘的万安东断裂带

    Figure 6. 

    图 7  位于南海西部陆缘的曾母西断裂带

    Figure 7. 

    图 8  西南次海盆和东部次海盆南部之间的中南-礼乐断裂带

    Figure 8. 

    图 9  马尼拉海沟俯冲带北段构造特征

    Figure 9. 

    图 10  南沙地震剖面选段示廷贾断裂

    Figure 10. 

    图 11  南沙海槽断裂与逆冲褶皱构造NS93-6地震测线

    Figure 11. 

    图 12  Kngh-2-N剖面示东部次海盆北部偏西边缘基底往海盆中心方向阶梯状下降

    Figure 12. 

    图 13  CT500剖面示西南次海盆北缘构造特征

    Figure 13. 

    图 14  南海块体构造分区图

    Figure 14. 

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收稿日期:  2023-07-07
修回日期:  2024-01-16
录用日期:  2024-01-16
网络出版日期:  2025-01-17

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